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Pumping-induced drawdown and stream depletion in a leaky aquifer system
James J Butler1, Xiaoyong Zhan, Vitaly A Zlotnik
1Kansas Geological Survey, 1930 Constant Avenue, Campus West, University of Kansas, Lawrence, KS 66047, USA. jbutler@kgs.ku.edu
Ground water pumping can impact streams, but models often assume impermeable layers. A new solution shows leakage through underlying layers is a key recharge source, especially for distant wells.
Area of Science:
- Hydrogeology
- Environmental Engineering
- Water Resources Management
Background:
- Groundwater pumping impacts streamflow, typically modeled using interconnected stream-aquifer systems.
- Existing models often assume an impermeable layer beneath the pumped aquifer, which may not reflect reality.
Purpose of the Study:
- Develop a semianalytic solution for drawdown and stream depletion that accounts for aquitard leakage.
- Investigate the role of aquitard leakage as a recharge mechanism in stream-aquifer systems.
Main Methods:
- Developed a new semianalytic solution for analyzing stream-aquifer interactions under pumping conditions.
- The solution does not require the assumption of an impermeable formation underlying the aquifer.
Main Results:
- Pumping-induced leakage through an underlying aquitard can be a significant recharge source.
- The importance of leakage increases with the distance between the pumping well and the stream.
- Ignoring aquitard leakage can lead to overestimations of drawdown and stream depletion.
Conclusions:
- Aquitard leakage is a crucial factor in stream-aquifer system assessments, even with low-transmissivity aquitards.
- Accurate estimation of aquitard properties is vital for effective water resources management and water rights adjudication.
- The new solution offers a versatile tool for practical assessments of pumping-induced stream-aquifer interactions, provided site-specific data support leakage.
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