Biogeochemical cycles - Powell County Schools
Download
Report
Transcript Biogeochemical cycles - Powell County Schools
Biogeochemical Cycles
Objectives:
Identify
and describe the flow of nutrients in
each biogeochemical cycle.
Explain the impact that humans have on the
biogeochemical cycles.
What Sustains Life on Earth?
Solar
energy,
the cycling of
matter, and
gravity sustain
the earth’s life.
Figure 3-7
Two Secrets of Survival:
Energy Flow and Matter Recycling
An
ecosystem
survives by a
combination of
energy flow and
matter recycling.
Figure 3-14
MATTER CYCLING IN
ECOSYSTEMS
Nutrient
Cycles: Global Recycling
Global Cycles called biogeochemical cycles, are
cycling of nutrients from the abiotic reservoirs
to biotic reservoirs.
Nutrients are the elements and compounds that
organisms need to live, grow, and reproduce.
Biogeochemical cycles move all nutrients
through air, water, soil, rock and living organisms
over millions of years.
MATTER CYCLING IN
ECOSYSTEMS
Nutrient
Cycles: Global Recycling
Abiotic – nonliving cycles like rock cycle, water
cycle and other chemical cycles.
Biotic – living organism involved cycles like
carbon and nitrogen cycle.
All cycles enable a specific chemical element or
nutrient to be taken and reused through various
forms.
What Sustains Life on Earth?
Figure 2
Closer look at cycles
WATER
CYCLE
Water’s Unique Properties
There
are strong forces of attraction between
molecules of water.
Water exists as a liquid over a wide
temperature range.
Liquid water changes temperature slowly.
It takes a large amount of energy for water to
evaporate.
Liquid water can dissolve a variety of
compounds including rock.
Water expands when it freezes.
Condensation
Rain clouds
Transpiration Evaporation
Transpiration
Precipitation
to land
from plants
Precipitation
Runoff
Surface runoff
(rapid)
Precipitation
Evaporation
from land Evaporation
from ocean
Precipitation
to ocean
Surface
runoff
(rapid)
Infiltration and
Percolation
Groundwater movement (slow)
Ocean storage
Fig. 3-26, p. 72
Effects of Human Activities
on Water Cycle
We
alter the water cycle by:
Withdrawing large amounts of freshwater from
the ground causing salt water to contaminate
reservoir.
Withdrawing large amounts from rivers and
streams changes flow of nutrients
Clearing vegetation causes eroding soils that
clogs streams.
Polluting surface and underground water.
All of this contributes to climate change.
Carbon Cycles:
One
of the most complex cycles on Earth.
Carbon Cycles:
Carbon
just like all other nutrients cycles from
one reservoir to another through many years.
Eg: Carbon enters plants as CO2 which is
incorporated into organic molecules by a
process called photosynthesis
When
organisms respire, a portion of
this carbon is returned to the
atmosphere as CO2.
Carbon Reservoir pools: Where
Carbon is stored
molecules – in living and dead
organisms.
Organic
Carbon
Dioxide (CO2) in atmosphere.
Organic matter in soil.
Fossil fuels and sedimentary rock like
limestone.
CO2 in ocean/water bodies.
Calcium carbonate in the shells of
marine organisms.
Effects of Human Activities
on Carbon Cycle
We
alter the carbon
cycle by adding
excess CO2 to the
atmosphere through:
Burning fossil fuels.
Clearing vegetation
faster than it is
replaced.
Just Breathing
Figure 3-28
The Nitrogen Cycle
Nitrogen
is the second largest nutrient cycle
on the planet, second only to carbon.
Effects of Human Activities
on the Nitrogen Cycle
We
alter the nitrogen cycle by:
Adding gases to atmosphere that contribute to
acid rain.
Adding nitrous oxide to the atmosphere through
farming practices which can warm the
atmosphere and deplete ozone.
Contaminating ground water from nitrate ions in
inorganic fertilizers.
Releasing nitrogen into the troposphere through
deforestation.
Effects of Human Activities
on the Nitrogen Cycle
Human
activities such
as production and
use of fertilizers now
“fix” (put into
environment) more
nitrogen than all
natural sources
combined.
Figure 3-30
Phosphorous Cycle
Phosphorous
Cycle has been greatly affected
by human activity in the last 100 years.
mining
excretion
Fertilizer
Guano
agriculture
uptake by
uptake by weathering
autotrophs
autotrophs
leaching, runoff
Dissolved
Land
Marine
Dissolved
in Soil Water,
Food
Food
in Ocean
Lakes, Rivers
Webs
Webs
Water
death,
death,
decomposition
decomposition
weathering
sedimentation
settling out
uplifting over
geologic time
Rocks
Marine Sediments
Fig. 3-31, p. 77
Effects of Human Activities
on the Phosphorous Cycle
We
remove large amounts of phosphate from
the earth to make fertilizer.
We reduce phosphorous in tropical soils
by clearing forests.
We add excess phosphates to aquatic
systems from runoff of animal wastes and
fertilizers.
Objectives:
STOP
Identify
and describe the flow of nutrients in
each biogeochemical cycle.
Explain the impact that humans have on the
biogeochemical cycles.
What Sustains Life on Earth?
Solar
energy,
the cycling of
matter, and
gravity sustain
the earth’s life.
Figure 3-7
Sulfur
trioxide
Water
Acidic fog and
precipitation
Sulfuric acid
Ammonia
Oxygen
Sulfur dioxide
Ammonium
sulfate
Hydrogen sulfide
Plants
Dimethyl
sulfide
Volcano
Industries
Animals
Ocean
Sulfate salts
Metallic
sulfide
deposits
Decaying matter
Sulfur
Hydrogen sulfide
Fig. 3-32, p. 78
Effects of Human Activities
on the Sulfur Cycle
We
add sulfur dioxide to the atmosphere by:
Burning coal and oil
Refining sulfur containing petroleum.
Convert sulfur-containing metallic ores into free
metals such as copper, lead, and zinc releasing
sulfur dioxide into the environment.
The Gaia Hypothesis:
Is the Earth Alive?
Some
have proposed that the earth’s various
forms of life control or at least influence its
chemical cycles and other earth-sustaining
processes.
The strong Gaia hypothesis: life controls the
earth’s life-sustaining processes.
The weak Gaia hypothesis: life influences the
earth’s life-sustaining processes.
What do you think?
Does
life on earth control earth’s lifesustaining processes or does life merely
influence these life-sustaining process?
FRQ Format.
Objectives:
Identify
and describe the flow of nutrients in
each biogeochemical cycle.
Explain the impact that humans have on the
biogeochemical cycles.