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Watersheds, Non-Point Pollution, and Hydrology Mr. Brian Oram, PG Professional Geologist, PASEO, Licensed Well Driller Lab Director, Center for Environmental Quality Wilkes University GeoEnvironmental Sciences and Engineering Department Wilkes Barre, PA 18766 http://www.water-research.net 7/7/2015 1 Center for Environmental Quality Non-profit/ equal opportunity employer, is operated and managed, within the GeoEnvironmental Sciences and Engineering Department Outreach Programs Environmental and Professional Education and Training Applied Research Community and Business Outreach Programs Website: http://www.water-research.net 7/7/2015 2 The Water Cycle 7/7/2015 3 What is a Watershed? The simple definition It's the area of land that catches rain and snow and drains or seeps into a marsh, stream, river, lake or groundwater. Right Now Your Sitting In a Watershed ! They cross county, state, and national boundaries (This is the challenge !) 7/7/2015 4 Watershed Map 7/7/2015 5 Watershed View 7/7/2015 6 Non Point Source Pollution Nonpoint source (NPS) pollution, unlike pollution from industrial and sewage treatment plants, comes from many diffuse sources. NPS pollution is caused by rainfall or snowmelt moving over and through the ground. As the runoff moves, it picks up and carries away natural and human-made pollutants, finally depositing them into lakes, rivers, wetlands, coastal waters, and even our underground sources of drinking water. These pollutants include: 7/7/2015 7 Sources of Non-Point Pollution Excess fertilizers, herbicides, and insecticides from agricultural lands and residential areas; Oil, grease, and toxic chemicals; Sediment from improperly managed construction sites, crop and forest lands, and eroding streambanks; Bacteria and nutrients from livestock, pet wastes, urban runoff and faulty septic systems; and Atmospheric deposition and hydromodification are also sources of nonpoint source pollution. 7/7/2015 We are Still the Largest Source of Oil Pollution to the Environment ! 8 Sources of Pollution Causes of Contamination Improper Waste Disposal Improper Well Construction Poor Site Selection Wells Not Properly Abandoned Improper Waste Storage Lack of Information on Hazardous Sites or Activities (Partial Listing) 7/7/2015 9 Primary Aquifers in PA 7/7/2015 10 Well Geology 7/7/2015 11 Surface Water & Groundwater 7/7/2015 12 Groundwater Pocono's Region Based on the geology of the Pocono's region, the Primary water quality problems are as follows: Corrosive Water Low pH Soft Water (low hardness) to Moderate Hardness Iron and Manganese Discolored Water – Reddish to Brown Tints Total Coliform Bacteria Sulfur Odors and Elevated Sulfates 7/7/2015 13 Coliform Bacteria Coliform Bacteria Absent or < 1 colony/100 ml Testing Purpose Used as an Indicator of Sanitary Condition of Water Source Sources Natural Soil Bacteria Human and Animal Waste Insect Waste 7/7/2015 14 Phosphate Phosphate will stimulate the growth of plankton and aquatic plants which provide food for larger organisms, including: zooplankton, fish, humans, and other mammals. Plankton represent the base of the food chain. Initially, this increased productivity will cause an increase in the fish population and overall biological diversity of the system. But as the phosphate loading continues and there is a build-up of phosphate in the lake or surfacewater ecosystem, the aging process of lake or surface water ecosystem will be accelerated. 7/7/2015 15 Phosphate Cycle 7/7/2015 16 Before and After 7/7/2015 17 Nitrate + Nitrite Drinking Water Standards(Primary) Nitrate: 10 mg as N/ L Nitrite: 1 mg N/L Health Concern Blue Baby Syndrome- Methemoglobinemia Sources Fertilizers Human and Animal Waste Non-anthropogenic sources (fixation, rock weathering) Atmospheric Deposition 7/7/2015 18 Nitrogen Cycle 7/7/2015 19 What Can We Do? Control Nutrient and Fertilizer Use Conserve Water Control Stormwater Runoff Properly Store and Handle Hazardous Waste Maintain Septic Systems Community Action and Education Monitoring 7/7/2015 20 Watersheds, Non-Point Pollution, and Hydrology Mr. Brian Oram, PG Professional Geologist, PASEO, Licensed Well Driller Lab Director, Center for Environmental Quality Wilkes University GeoEnvironmental Sciences and Engineering Department Wilkes Barre, PA 18766 http://www.water-research.net 7/7/2015 21 Groundwater Moves 1. Which ways can groundwater move? a. Up b. Down c. Sideways d. All of the above 1. d. All of the above Although most movement is lateral (sideways), it can move straight up or down. Groundwater simply follows the path of least resistance by moving from higher pressure zones to lower pressure zones. 7/7/2015 22 Groundwater Moves 2. How is the speed of groundwater movement measured? a. Feet per day b. Feet per week c. Feet per month d. Feet per year 2. d. Feet per year Groundwater movement is usually measured in feet per year. This is why a pollutant that enters groundwater requires many years before it purifies itself or is carried to a monitored well. 7/7/2015 23 Groundwater Moves 3. How is stream flow usually measured? a. Feet per second b. Feet per minute c. Feet per hour d. Yards per hour 3. a. Feet per second Water flow in streams/rivers is measured in feet per second. 7/7/2015 24 Groundwater Moves 4. What determines how fast groundwater moves? a. Temperature b. Air pressure c. Depth of water table d. Size of materials 4. d. Size of materials Coarse materials like sand and gravel allow water to move rapidly. (They also form excellent aquifers because of their holding capacity.) In contrast, finegrained materials, like clay or shale, are very difficult for water to move through. Thus, water moves very, very slowly in these materials. 7/7/2015 25 Groundwater Moves 5. Can the water table elevation change often? a. Yes b. No 5. a. Yes Water table elevations often fluctuate because of recharge and discharge variations. They generally peak in the winter and spring due to recharge from rains and snow melt. Throughout the summer the water table commonly declines due to evaporation, uptake by plants (transpiration), increased public use, industrial use, and crop, golf course and lawn irrigation. Elevations commonly reach their lowest point in early fall. 7/7/2015 26 Groundwater Moves 6. Does aquifer storage capacity vary? a. Yes b. No 6. a. Yes Just like the water level in rivers and streams, the amount of water in the groundwater supply can vary due to seasonal, weather, use and other factors. 7/7/2015 27 Watersheds, Non-Point Pollution, and Hydrology Mr. Brian Oram, PG Professional Geologist, PASEO, Licensed Well Driller Lab Director, Center for Environmental Quality Wilkes University GeoEnvironmental Sciences and Engineering Department Wilkes Barre, PA 18766 http://wilkes.edu/~gse 7/7/2015 28 Private Water Supply A Pennsylvania Perspective Mr. Brian Oram, PG Professional Geologist, PASEO, Licensed Well Driller Lab Director, Center for Environmental Quality Wilkes University GeoEnvironmental Sciences and Engineering Department Wilkes Barre, PA 18766 http://wilkes.edu/~gse 7/7/2015 29 Center for Environmental Quality Non-profit/ equal opportunity employer, is operated and managed, within the GeoEnvironmental Sciences and Engineering Department Outreach Programs Environmental and Professional Education and Training Applied Research Community and Business Outreach Programs Website: http://wilkes.edu/~eqc 7/7/2015 30 Keys to a Safe Drinking Water The Sanitary Survey- Proper Site Location State Federal and Local Regulations Types of Well Water Sources Well Drilling and Construction Initial Water Testing Well Water Conditioning or Treatment Well Maintenance 7/7/2015 31 Protect Your Water Source Things You or Your Community Can Do Periodically Inspect Proper Abandonment Drain Surface Water Away Chemical Storage, Install Sanitary Seal Disposal and Use Annual Testing Keep Wellhead Above Grade Maintain Records Proper Well Location Start a Community Based Septic System Groundwater Education Maintenance Program Recycle used Oil and Participate in Hazardous Chemical Disposal Programs 7/7/2015 32 Why Test My Water ? A USGS survey found that 70% of private wells were contaminated. This contamination could result in acute or chronic health concerns. In general, there are no regulations related to well construction, placement, or required testing. It is up to you to determine the safety of your water. EPA recommends, at minimum, an annual water test for private wells. 7/7/2015 33 Drinking Water Regulations The Safe Drinking Water Act (SDWA), passed in 1974 and amended in 1986 and 1996, gives the Environmental Protection Agency (EPA) the authority to set drinking water standards. These standards are divided into two broad categories: Primary Standards (NPDWR) and Secondary Standards (NSDWR). 7/7/2015 34 Primary Standards (NPDWR) National Primary Drinking Water Regulations Primary standards protect drinking water quality by limiting the levels of specific contaminants that can adversely affect public health and are known or anticipated to occur in water. They take the form of Maximum Contaminant Levels or Treatment Techniques. There are over 100 chemical and biological primary drinking water standards, which include: trace metals, disinfection agents, disinfection byproducts, radiological, microbiological agents, and organic chemicals. Examples: Arsenic, Lead, MTBE, total coliform, Giardia, Trihalomethanes, Asbestos, Copper, Benzene, Trichloroethane, etc. 7/7/2015 35 Secondary Standards National Secondary Drinking Water Regulations These standards were established more for cosmetic effects (such as skin or tooth discoloration) or aesthetic effects (such as taste, odor or color) in drinking water. The secondary standards include: aluminum, chloride, color, corrosivity, fluoride, foaming agents, iron, manganese, odor, pH, silver, sulfate, total dissolved solids, and zinc. 7/7/2015 36 What Should I Test The Selection of the Appropriate Testing Parameters Depends on YOUR Water How does it taste? Do you have odor problems ? Are there any aesthetic problems, such as: color, turbidity, grittiness, or staining ? Where are you located ? How much do you want to spend ? Comprehensive testing can cost over $2500.00 7/7/2015 37 Taste Problems Salty or Brackish Taste Alkali Taste Corrosion, Low pH, high metallic content (Cu, Fe, Mn, Pb,Al, Zn) Metallic or Bitter Taste 7/7/2015 High Sodium Elevated Hardness or alkalinity 38 Odors Rotten Egg / Musty Odor Oily Methane Smell Chemical/ Solvent 7/7/2015 Sulfate, Sulfur, Nuisance Bacteria Gasoline, Oil Contamination or Nuisance Bacteria Organic Material or Natural Gas Industrial Chemicals 39 Sediments and Stains Milky or Cloudy Precipitation of carbonates / sulfates, excessive air, suspended solids, aquifer material Bluish Green – Green Precipitates Copper, hardness, aggressive water and corrosion by-products, nuisance bacteria Blackish Tint or Black Slimes Reactions with manganese and possibly iron, nuisance bacteria Yellowish or Reddish Tint or Slimes Humic material, dissolved or precipitated iron, nuisance bacteria 7/7/2015 40 Impacts Water Supply Land-use Residential (Rural or Urban) Industrial Agricultural Commercial Undeveloped Woodland Water Source Well, Spring, Cistern, Dug Well Water Characteristics Geology Well Construction and Age Distribution System Type / Age 7/7/2015 Known Hazards Areas Waste Disposal Sites Chemical Storage Chemical Spills Underground Storage Pipelines Sewage and Sludge Disposal Surrounding Water Users Well Construction Well Spacing Water Withdrawal Recharge Areas 41 Groundwater Pocono's Region Based on the geology of the Pocono's region, the Primary water quality problems are as follows: Corrosive Water Low pH Soft Water (low hardness) to Moderate Hardness Iron and Manganese Discolored Water – Reddish to Brown Tints Total Coliform Bacteria Sulfur Odors and Elevated Sulfates 7/7/2015 42 Less Common Problems These water quality are not common to Groundwater in Pocono's Region. Elevated Nitrate- Nitrite Levels Radon or Radiological Organic Contamination Elevated Trace Metals (except corrosion by-products like Copper, Lead, Aluminum, Zinc) Salty or Brackish Water (some areas) Trihalomethanes Pathogenic Organisms 7/7/2015 43 Coliform Bacteria Coliform Bacteria Absent or < 1 colony/100 ml Testing Purpose Used as an Indicator of Sanitary Condition of Water Source Sources Natural Soil Bacteria Human and Animal Waste Insect Waste 7/7/2015 44 Corrosive Water Chemical or Biochemical Reaction between the water and metal surfaces. The corrosion process is an oxidation/reduction reaction that returns refined or processed metal to their more stable ore state. Corrosion can also be accelerated by: 1) low pH; 2) high flow rate within the piping; 3) high water temperature; 4) Chemistry of the water; and 4) presence of suspended solids, such as sand. 7/7/2015 45 Evidence of Corrosion Physical Signs of Corrosion Leaky Pipes Water Has Bitter Taste Greenish Blue Stains Red or Discolored Water Premature Failure of Water Heaters/ Heat Exchange Units Elevated Levels of Copper, Lead, Aluminum, Zinc, Iron, Chromium 7/7/2015 Check for Corrosion Testing for Cu and Pb and other metals and TDS Corrosivity Testing – Saturation Index Nuisance Bacteria Testing 46 pH pH < 7 acidic a pH > 7 basic NSDWR – 6.5 – 8.5 Problems Bitter or Alkali Taste Corrosion Scale Formation Leaching Metals 7/7/2015 47 Water Hardness The hardness of a water is a measure of the concentration of the multivalent cations (Ca, Mg, Fe, Mn, etc) associated with carbonates (CO3) . Hardness is typically reported as mg /L as CaCO3 (calcium carbonate) Grains per gallon (1 gpg (US) = 17.12 mg CaCO3/L ). Hardness Classification: – Soft: 0 to 17 mg CaCO3/L – Slightly Hard: 17 to 60 mg/L; – Moderately Hard 60 to 120 mg/L – Hard 120 to 180 mg/L – Very Hard > 180 mg/L 7/7/2015 48 Nitrate + Nitrite Drinking Water Standards(Primary) Nitrate: 10 mg as N/ L Nitrite: 1 mg N/L Health Concern Blue Baby Syndrome- Methemoglobinemia Sources Fertilizers Human and Animal Waste Non-anthropogenic sources (fixation, rock weathering) Atmospheric Deposition 7/7/2015 49 Nitrogen Cycle 7/7/2015 50 Sulfates in Water Sulfates are a combination of sulfur and oxygen and are a part of naturally occurring minerals in some soil and rock formations that contain groundwater. The mineral dissolves over time and is released into groundwater. Hydrogen sulfide gas also occurs naturally in some groundwater. The gas is formed from decomposition of organic compounds contained within the bedrock. Problems are typically found in aquifers that are shale, siltstone, peat related, or near surface sources of organic material. Sulfur-reducing bacteria, use sulfur as an energy source and are the primary producers of large quantities of hydrogen sulfide. These bacteria chemically change natural sulfates in water to hydrogen sulfide 7/7/2015 51 Problems with Sulfates NSDWR Laxative Effect- MCL 250 mg/L Form Precipitates on Piping and Fixtures Rotten Egg Odors Sewage Gas Odors Corrosion Water Heater Failure/Odors 7/7/2015 52 Summary Keys to Safe Drinking Water (Private Well) Proper Handling of Chemicals and Waste Development of Local Standards Understand Your Source Annual Water Testing Public Education 7/7/2015 53 Private Water Supply A Pennsylvania Perspective Mr. Brian Oram, PG Professional Geologist, PASEO, Licensed Well Driller Lab Director, Center for Environmental Quality Wilkes University GeoEnvironmental Sciences and Engineering Department Wilkes Barre, PA 18766 http://wilkes.edu/~eqc http://wilkes.edu/~gse 7/7/2015 54