Propagation of solutes and pressure into aquifers following river stage rise
Water level rises associated with river flow events induce both pressure and solute movement into adjacent aquifers at vastly different rates. We present a simple analytical solution that relates the travel time and travel distance of solutes into an aquifer following river stage rise to aquifer pro...
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Veröffentlicht in: | Water resources research 2013-09, Vol.49 (9), p.5246-5259 |
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Format: | Artikel |
Sprache: | eng |
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