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Transient Flow to a Large-Diameter Well in an Aquifer With Storative Semiconfining Layers

✍ Scribed by Moench, Allen F.


Book ID
119737710
Publisher
American Geophysical Union
Year
1985
Tongue
English
Weight
931 KB
Volume
21
Category
Article
ISSN
0043-1397

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Radial groundwater flow to a finite diam
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## Abstract A mathematical model that describes the drawdown due to constant pumpage from a finite radius well in a two‐zone leaky confined aquifer system is presented. The aquifer system is overlain by an aquitard and underlain by an impermeable formation. A skin zone of constant thickness exists