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FIGURES 1. Block diagram showing the generalized geologic setting for glacial-drift, river-valley aquifers 4 Contents III 2. Block diagram showing recharge-discharge relations and flow patterns in glacial-drift, river-valley aquifers 5 3-5. Diagrams showing groundwater flow at various stages of aquifer development: 3. Natural equilibrium conditions before pumping 6 4. Early pumping conditions 6 5. Late pumping conditions at equilibrium 6 6. Diagram of a pumping well showing a cross-sectional view of the cone of depression and a plan view of the area of influence 7 7. Diagram of a pumping well showing a cross-sectional view of the zone of contribution and a plan view of the contributing area 8 8. Block diagram showing the geohydrologic features of the hypothetical aquifer used in figure 9 to illustrate the difference between the area of influence and the contributing area of a pumped well 8 9. Maps of the hypothetical aquifer, illustrated in figure 8, showing prepumping flow net, steady-state drawdowns and the area of influence of a pumped well, and flow net and contributing area for pumping conditions 10 10-12. Diagrams showing: 10. A, Head distribution for a natural-flow system; fi, Drawdowns caused by a pumping stress; and C, Head distribution resulting from superposition of A and B 11 11. The geohydrologic features of the hypothetical stratified-drift, rivervalley aquifer addressed in the model analyses 13 12. An idealized version of the aquifer for analysis with an analytical model using a line-source river boundary 15 13. Maps of the idealized aquifer showing, A, Prepumping water-table altitudes; B, Drawdowns computed by using the analytical model; and C, Water-table altitudes and contributing area resulting from superposition of A and B for the line-source river-boundary condition 16 14. Finite-difference grid used for the two-dimensional numerical-model analyses shown in plan and cross-sectional views 17 15-17. Maps showing: 15. Contributing areas for a well pumping 0.25 million gallons per day in a river-valley aquifer 18 16. Average steady-state water-table altitudes, without pumping, computed by using the two-dimensional numerical model 19 17. Water-table altitudes and contributing areas of a well pumped at 0.5, 1.0, and 2.0 million gallons per day 20 18. Graphs showing sizes of contributing areas and sources of water pumped from the well as a function of well discharge 21 19. Maps showing water-table altitudes and contributing areas of a well pumped at 1.0 million gallons per day for 0.5 times average, average, and 1.5 times average recharge 23 20. Graphs showing sizes of contributing areas and sources of water pumped from the well as a function of recharge rate 24 21. Maps showing water-table configuration and contributing area of a well pumped at 1.0 million gallons per day after 30, 90, and 180 days of drought 25 22. Maps showing water-table altitudes and contributing areas of a well pumped at 1.0 million gallons per day and having streambed coefficients (k'lb'} of 0.1, 1.0, and 10.0 26 23. Graphs s...
This general-interest report appraises the occurrence, source, flow, and quality of ground water in Rhode Island. Ground water, withdrawn from all major geologic units in Rhode Island, provided drinking water for about one-fourth of the State's population in 1985.Ground water, mostly unconfined, is found in unconsolidated glacial till and stratified drift and in the underlying fractured bedrock. Thick deposits of stratified sand and gravel are the most productive aquifers in the State for public supply. Most private wells tap bedrock aquifers.Ground water flows from upland recharge areas toward valley discharge areas. Most of the land surface is a recharge area. Large-capacity wells, located in permeable sediments near streams, commonly induce surface water to flow from streams into aquifers.Concentrations of dissolved solids in ground water are generally less than 200 milligrams per liter, as compared to the National Secondary Drinking-Water Regulation of 500 milligrams per liter. Natural contaminants include iron, manganese, and radon. Withdrawals in coastal areas have caused saltwater intrusion.Waste-disposal sites, industrial spills, leaking underground storage tanks, road salt, agricultural chemicals, and septic systems have contaminated ground water at some locations with metals, nitrate, bacteria, radionuclides, excessive concentrations of common ions, and more than 50 synthetic organic chemicals and petroleum products. Contamination by volatile organic compounds has been the major cause of public-well closings.The rural Pawcatuck River basin contains nine high-yield stratifieddrift aquifers. Southeastern Rhode Island, covered by clayey till, has no major aquifers. Stratified-drift aquifers in urbanized northeastern Rhode Island have a large potential yield but many water-quality problems. Rural western areas depend on ground water. Purpose and Scope of the ReportThis report provides Rhode Island's citizens with a broad overview of the State's ground-water resources and ground-water-contamination problems. The intended audience includes interested citizens, teachers, State and local government boards and agencies, and private organizations involved in water-resources issues.The following questions were posed in developing the report: * What is the importance of ground water in Rhode Island? * What is ground water? * Where does it come from? * Where does it go? * How does ground water become contaminated? * Where are the major ground-water resources and contamination problems in Rhode Island?
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