by Thomas E. Reilly and David W. Pollack
Abstract
Introduction
Areas Contributing Recharge and Sources of Water to
Wells
Previous Related Work
Factors Affecting Areas Contributing Recharge to Wells
Method of Analysis
Delineation of Areas Contributing Recharge to Wells in
Hypothetical Ground-Water Systems
Case 1-Homogeneous System
Well Discharge of 2,000 Cubic Feet per Day from Three Different
Screened Intervals
Well Discharge of 10,000 Cubic Feet per Day from Three
Different Screened Intervals
Well Discharge of 30,000 Cubic Feet per Day
Well Discharge of 30,000 Cubic Feet per Day in the Presence of
an Additional Well Discharging 130,000 Cubic Feet per Day
Case 2-Low-Hydraulic-Conductivity Local Confining Unit
Case 3-High-Hydraulic-Conductivity Units
Case 4-Random Distribution of Hydraulic Conductivity
Discussion of Simulation Results
Considerations for the Protection of Ground Water
References Cited
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