Transcript Gabriel Kasozi - Soil and Water Science
Slide 1
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 2
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 3
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 4
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 5
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 6
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 7
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 8
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 9
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 10
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 11
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 12
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 13
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 14
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 15
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 16
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 17
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 18
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 19
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 20
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 21
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 22
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 23
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 2
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 3
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 4
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 5
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 6
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 7
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 8
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 9
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 10
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 11
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 12
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 13
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 14
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 15
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 16
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 17
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 18
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 19
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 20
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 21
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 22
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris
Slide 23
CHARACTERIZATION OF SORPTION
AND DEGRADATION OF ORGANIC
PESTICIDES APPLIED TO
CARBONATIC SOILS
Gabriel Nuffield Kasozi
Source: usda.gov
Outline
Introduction
Hypothesis
Objective of the study
Materials and Methods
Preliminary results
Introduction
Carbonatic soils are composed of
more than 40% Carbonates
Over 500 carbonatic soils in USA and
12 are in South Florida
85% of Florida vegetables and
Tropical fruits grown on Carbonatic
soils
Source: BMP project report, 2002
Pesticide use
Estimated Annual Total Pesticides Use in SFWMD
14,590 tons .
Pesticides Detected in Water Resources in South FL and PR
1
Pesticide
Chemical class
Where detected
Atrazine
S-triazine
Ground, surface water (FL; PR) 1,2,4
Ametryne
S-triazine
Ground, surface water (FL; PR) 3,4
Diuron
Substituted urea
Surface water (FL) 1
Endosulfan
Organochlorine
Surface water (FL)
Enthroprop
Organophosphate
Surface, ground water (PR) 3
Diazinon
organophosphate
Surface, ground water (PR) 3
Lindane
organochlorine
Surface, ground water (PR) 3
Miles and Pfeuffer (1997); 2 Potter et al., (2002); 3 Dumas and Rosario (2003); 4 CondeCostas and Rodriguez (1997); FL= Florida; PR = Puerto Rico
Dade Hydrogeologic Cross-section
Introduction
Sorption and degradation determine the fate
of an applied organic pesticide
Source: SFWMD
Hypothesis
Organic pesticides are adsorbed less
on carbonatic soils as compared to
non-carbonatic soils
The nature of soil organic matter affects
the degree of pesticide sorption
Pesticides degrade faster in Carbonatic
soils than in non-carbonatic soils
Objective of the study
Characterize and compare chemical and
physical properties of carbonatic soils
with those of associated non-carbonatic
soils and soils from other areas
Characterize sorption and degradation of
selected pesticides and create a database
for sorption and transformation of these
pesticides on carbonatic soils
Objective of the study
Characterize organic matter (formation,
composition and functionality)
Identify the dominant component
controlling sorption of pesticides
Materials and Methods
Soils
• Soil samples will be taken from South Florida,
Puerto Rico and Uganda
• Biscayne, Perrine, Pennsuco, Chekika, Krome,
Lauderhill, Tamiami
Proposed Pesticides
• Atrazine, Ametryne, Oxamyl, Diuron,
Endosulfan, Lindane, Carbaryl, Enthroprop,
Diazinon
Materials
Experiment 1
• Characterization of soil physical and
chemical properties
• pH, TOC, CEC, Clay Minerals, CaCO3
• Determination of organic carbon
• Walkley-Black method
• Thermogravimetry
• Sorption isotherms determination (Batch
slurry method)
Methods
Experiment 2
• Characterization of organic matter
• Stable isotope δ 13C, δ 15N, and C/N
ratios
• n-Alkanes by GC-FID
13
1
• Liquid and Solid state C and H
NMR
• Pyrolysis GC-MS
Materials and Methods
Experiment 3
Characterization of the nature of binding
existing between OM and pesticides
• 13C NMR
• NanoESI-GC-MS
• Flow Calorimetry
Materials and Methods
Experiment 4
Characterization of degradation of pesticides
in carbonatic soils
Solvent extractable disappearance of the
parent pesticide
Degradation rate coefficients and halflife (t1/2) will be determined
Materials and Methods
Data Analysis
Sorption data will be fit using the
Freundlich model
Degradation data will be fit using first
order kinetics
Preliminary Results
Table of results
Soil
ε
% CaCO3
Π
% OC
ε
% OM
Biscayne
Perrine
80
87
5.82
2.79
9.82
4.75
Pennsuco
Krome
Chekika
LauderHill
67
87
-
2.37
1.45
1.9
35.78
3.45
3.94
-
Tamiami
-
36.25
-
Matecumbe
-
28.13
-
= Walkley and Black ; Π = Thermogravimetry
Π
Preliminary Results
TG % OM vs WB % OC
12.00
TG (%OM)
10.00
y = 1.755x
R2 = 0.9514
8.00
6.00
4.00
2.00
0.00
0.00
1.00
2.00
3.00
4.00
5.00
WALKLEY-BLACK (%OC)
6.00
7.00
Comparison of
TG with
Walkley-Black
for OC
determination
Literature
Conversion
factor: 1.724
Preliminary Results
Table of results
Soil
Biscayne
Perrine
Krome
Chekika
Lauderhill
Soil solution ratio: 1:2
pH (KCl)
(1 M)
7.66
7.78
7.59
7.72
6.98
pH (H2O)
8.11
8.00
8.51
8.29
7.39
Preliminary Results
Linear Sorption Isotherm for Biscayne
Diuron Isotherm (Biscayne)
ADSORBED CONC. (μg/g) )
40
y = 5.84x
R2 = 0.9805
35
30
25
20
15
10
5
0
0
1
2
3
4
SOLUTION CONC. (μg/m l)
5
6
7
Preliminary Results
Linear Sorption Isotherm for Krome
Diuron Isotherm (Krome)
ADSORBED CONC. (μg/g) )
25
y = 3.11x
R2 = 0.9516
20
15
10
5
0
0
1
2
3
4
5
SOLUTION CONC. (μg/m l)
6
7
8
Preliminary Results
Sorption coefficients of Diuron
Soil series
Sorption coefficient
KD
Koc
Biscayne
5.84
101
Perrine
2.6
92
Chekika
2.6
136
Krome
3.11
222
Lauderhill
139.49
390
Iowa
11.09
240
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
400 †
Preliminary Results
Sorption coefficients of Atrazine
Soil series
Sorption ceofficient
KD
Koc
Biscayne
2.16
37
Perrine
0.71
29
Chekika
0.76
40
Krome
0.82
57
Lauderhill
45.20
101
Iowa
4.06
88
† Literature
†(Wauchope et al., 1992, and Nkedi-Kizza et al., 1985)
100 †
Advisory Committee:
Dr. Peter Nkedi-Kizza
Dr. Yucong Li
Dr. David Hodell
Dr. David Powell
Dr. Willie Harris