DNAPL migration through a fractured perching layer

The migration of a DNAPL (TCA) was demonstrated by a laboratory flow visualization experiment. The system consists of two unconfined aquifers separated by a siltstone perching layer containing a single fracture that conducts water flow downward. The TCA migrated along a tortuous path in the upper sa...

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Veröffentlicht in:Ground Water 1998-07, Vol.36 (4), p.605-610
Hauptverfasser: Stephens, D.B. (Daniel B. Stephens and Associates Inc., Albuquerque, NM.), Kelsey, J.A, Prieksat, M.A, Piepho, M.G, Shan, C, Ankeny, M.D
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Sprache:eng
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