GROUNDWATER. Water Resources of NYS: The Nature of its Underground Water. Composite Groundwater Environment. Groundwater Resources of NYS

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Water Resources of NYS: The Nature of its Underground Water Prof. Anthony Grande AFG 2014 1 GROUNDWATER Groundwater - water occupying the pore spaces and cracks in rocks and unconsolidated material. The best groundwater is found in sand and gravel formations. top of the groundwater; varies in depth from the surface with water supply. Dependency on groundwater (wells) is greatest in rural areas. But, the largest area of the state that uses groundwater is Long Island and the greatest number of people in the US who are dependent on it are in Nassau and Suffolk counties. 2 Composite Groundwater Environment Groundwater Resources of NYS Horizontal and vertical joints in the crystalline bedrock trap water. 3 <Potentially highly productive <Intensively used water supply <Critical water supply Source: NYS DEC 4 Potential Pesticide Exposure from Groundwater Marcellus Shale Formation Southern Tier, Finger Lakes and Catskills Map of all pesticide use as compiled by Soil and Water Lab at Cornell University. 5 <<Active wells <<NYC watershed <<Catskill Forest Preserve <<Marcellus zone <<Counties producing gas 6 1

Marcellus Shale Controversy What are the chief ISSUES? Effect on water supply. Effect on the environment. Effect on aquifers and streams Water volume needed Water management Effect on NYC drinking water Seismic events (pressurized water) Air and water contamination (from air release of gases and surface/underground water spills) Safety of fracking fluids Waste water (movement/storage) Release of radiation into air Effect on Catskill Forest Preserve Exploration bandwagon (don t miss out on the trend before new sources/technology are found) Property values (increase or decrease) Tax revenue (state, county, town) Income streams from exploration (leases, rentals, sales, jobs, support services) Price of natural gas/cf (present/future) Fracking the Shale Hydraulic fracturing of shale layers to release natural gas is done by inserting water and chemicals under high pressure. Contamination of groundwater and air is a possible side effect. Fracking Site Effect on the economy. 7 8 Protecting Groundwater from Fracking http://www.dec.ny.gov/docs/materials_minerals_ pdf/gwprotection.pdf 2011 DEC Proposal to Prohibit Fracking in Sensitive Areas http://www.nytimes.com/interactive/us/drilling_ DOWN_SERIES.html http://www.nytimes.com/interactive/2011/03/01/us/ch emicals-and-toxic-materials-in-hydrofracking.html Oct 1, 2012: http://www.nytimes.com/2012/10/01/nyregion/withnew-delays-a-growing-sense-that-gov-andrewcuomo-will-not-approve-gasdrilling.html?ref=nyregion&_r=0 Sept 30, 2012: http://www.nytimes.com/2012/09/30/realestate/fracki ng-fears-hurt-second-home-sales-incatskills.html?pagewanted=all Oct. 25, 2013: www.mintpressnews.com/new-york-court-of-appealsfracking/171239/print Jan. 29, 2014: www.bloomberg.com/news/print/2014-01-29/newyork-decision-on-fracking-regulations-delayed.html 9 Map was part of a Sept., 2011 NYSDEC environmental impact statement report on hydraulic fracturing. 10 Local Movements and Fracking Local Movements and Fracking Map From Wall Street Journal 11 12 2

L I Groundwater Situation Physical Make-up of Long Island LI is the largest populated area of the country that depends exclusively on groundwater. It is rapidly urbanizing. There are no dependable surface water sites to supply fresh water to the residential, industrial and agricultural sites. Long Island is surrounded by salt water. The NYC Water Supply system does not have enough water to share with LI without drastically enlarging the Catskill collection system. Created by glaciers. Porous unconsolidated material (sand, silt, clay and gravel) form layers that hold water. Bedrock deeply buried. Receives about 44 in. of precipitation annually. Surrounded by salt water. There are 4 aquifers: -Upper Glacial -Jameco -Magothy -Lloyd There are 2 aquicludes: -Gardiners Clay -Raritan Clay The depth of the water table varies locally with the rates of withdrawal and recharge. 13 14 Major Units of the Long Island Aquifer Layers of Long Island: Upper Glacial Aquifer (youngest layer) Gardiners Clay Jameco Aquifer Long Island Water Towers Continental Basement Rock Magothy Aquifer Raritan Clay Lloyd Aquifer Bedrock Jones Beach Water Tower, encased in a brick building, is supplied by 4 wells over 1000 feet deep. Copyright 2008 New York State Department of Environmental Conservation 15 16 Problems Facing LI Groundwater Freshwater area (lens) under LI is shrinking. Surface area for freshwater recharge has gotten smaller. The water table is being lowered (more pumping and less recharge). Reduction in outward pressure is allowing salt water to move inland. Surface pollution has contaminated groundwater closest to the surface. Rising sea level will submerge more coastal areas, reducing recharge and contaminating freshwater. 17 Land Use and its Effect on Groundwater Level. SUBURBAN COMMUNITY RURAL LOW DENSITY INDUSTRIAL 18 3

Lowering of the Water Table Island Hydrogeology: Schematic of a Freshwater Lens with a Saltwater Interface Source: Fayette Co., TX 19 Source: US EPA 20 Saltwater Interface The interface moves landward with increased freshwater withdrawal. Decreased withdrawal and/or pressurized recharge can stop it. Groundwater Recharge Basin Rainwater needs to be collected to replenish withdrawals since groundwater is the sole source of freshwater for the people who live on Long Island outside of NYC, Open space, storm water collection and the return of treated waste water are ways to help replace removed ground-water. Fresh water Salt water Recharge Basin PARK Source: USGS Circular 1262 21 This is an example of non-pressurized or natural recharge by seepage. 22 Waste Water Disposal Septic System vs. Cesspool Septic System separates solid waste from waste water. Waste water is directed to an underground drainage field for dispersal. Holding tank needs to be cleaned out. Cesspool tank fills with waste water and solids. Water is slowly released to surrounding soil. Solids have to be pumped 23out. Ensuring a Safe Yield on LI Problem Remedy Increased use >>Conservation; regulate consumption Suburbanization >>Preserve open space; restore wetlands Over pumping >>State regulation Contamination >> Regulation of land fills, cesspools, septic tanks, industry and agriculture Replenishment >>Required recharge basins; open space Loss of run off >>Move to sanitary sewers, collection/seepage ponds Irrigated farmland >>Water conservation methods; hybrid plants Salt water intrusion >>Reduced pumping; pressurized recharge 24 4

NEXT The Coastal Zone 25 5