View Original Image at Full SizeFigure 35. Schematic cross-section showing effects of pumping and generation of a cone of depression in an unconfined aquifer between a lake and a stream. Pumping and the ensuing cone of depression reverse the hydraulic gradient from pre-development (A) and induce flow from the stream into the groundwater system and to the well (B).
Originally uploaded in Integrate:Teaching for Sustainability:InTeGrate Modules:Water Science and Society:Student Materials.
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Mar28 17
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- Effects of Pumping Wells
https://serc.carleton.edu/integrate/teaching_materials/water_science_society/student_materials/929
Provenance
Source: USGS: Ground water in the Great Lakes Basin: the case of southeastern Wisconsin
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