Resolving the Stream Depletion Model Paradox: Theory of Depletion with Stream Drawdown near a Pumping Well

Abstract

Link to supplemental material on publisher website: https://ngwa.onlinelibrary.wiley.com/action/downloadSupplement?doi=10.1111%2Fgwat.13425 &file=gwat13425-sup-0001-supinfo.pdf 2 Article Impact Statement: Streams have finite capacity to store water and undergo transient drawdown and depletion when a hydraulically connected aquifer is pumped.