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Die Kenntnis der hydraulischen Durchlässigkeit (kf-Wert) ist die Grundvoraussetzung für das Prozessverständnis der Grundwasserbewegungen im Untergrund. Daher existieren zahlreiche Labor- und Feldmethoden zur Bestimmung der hydraulischen Durchlässigkeit, deren Anwendung allerdings zu deutlich unterschiedlichen kf-Werten führen kann. Zur Quantifizierung dieser Variabilität wurde der kf-Wert eines Quarzsandes...
A modified version of a published slug test model for unconfined aquifers is applied to cross-hole slug test data collected in field tests conducted at the Widen site in Switzerland. The model accounts for water-table effects using the linearized kinematic condition. The model also accounts for inertial effects in source and observation wells. The primary objective of this work is to demonstrate applicability...
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