Groundwater and Wells: An Introductory Discussion with Application to Northeastern Illinois H. Allen Wehrmann, P.E. Illinois State Water Survey Illinois Department of Natural Resources 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Topical Presentation Outline Basic Concepts and Definition The Hydrologic Cycle What Is Groundwater? Concepts and Definitions Porous Flow vs. Fractured Flow Aquifers vs. Aquitards Artesian vs. Water Table Conditions Regional Groundwater G Flow Systems S Well and Aquifer Hydraulics 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future The Water Cycle Climate, surface water, and groundwater are linked 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Porous Systems Groundwater flows through pore spaces between grains 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Fractured Systems 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Fractured Limestone or Dolomite 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Aquifers vs. Aquitards An aquifer is a saturated bed, formation, or group of formations that yields water in sufficient quantity to be of consequence as a source of supply. An aquitard yields inappreciable quantities of water, but leakage of water through the aquitard is possible. Aquitards often act as confining beds. 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Unconfined vs. Confined Groundwater An unconfined aquifer is one in which groundwater possesses a free surface open to the atmosphere. The upper surface of the zone of saturation is called the water table. A confined fi d aquifer if is i one iin which hi h groundwater d t iis confined under pressure by overlying and underlying aquitards or aquicludes, and water levels in wells rise above b th the ttop off the th aquifer. if A confined fi d aquifer if is i also l called an artesian aquifer. 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Unconfined Aquifers Land Surface Unsaturated ((Vadose)) Zone Water Table Saturated Zone Unconfined Aquifer Bedrock 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Confined Aquifers Land Surface Unsaturated (Vadose) Zone Water Table Unconfined Aquifer Saturated Zone Potentiometric Surface Confining Layer - Aquitard Confined Aquifer Bedrock 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Confined Aquifers and Artesian Wells Flowing artesian well Land surface Confining layer Confined Aquifer f 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Regional Groundwater Flow Systems 0.1 mile 20 miles Depth 0’ 100’ 10’ 200’ 20’ 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Cone of Depression 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Overlapping Cones of Depression 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Overlapping Cones of Depression: Well Interference 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Overlapping Cones of Depression: Well Interference 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Overlapping Cones of Depression: Well Interference 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Overlapping Cones of Depression: Well Interference 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Potentiometric S f Surface off the th Deep Bedrock A if S Aquifer System, t Fall 2000 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Potentiometric Surface across NE Illinois WEST EAST Elevation (ft) Elevation (ft) 1000 1000 DeKalb 800 Elburn Geneva 800 Elmhurst Bellwood Industrial site in Chi cago 600 600 400 400 200 200 0 St. Peter 0 Ss - 200 -200 - 400 -400 - 600 - 800 Ironton -Galesviil le Ss -600 -800 -1000 -1000 -1200 -1200 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Deep Well Water Levels Levels, Cook County 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Deep Well Water Levels, Kendall County 600 Ellevation abov ve Sea Level (feet) 500 400 300 200 100 Oswego #3 0 1950 1960 1970 1980 1990 2000 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future Water Sources for Public Supply in Northeast Illinois 2007 Priority Places Workshop: Implementing a Sustainable Water Supply for Kane County’s Future
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