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Ground Water ; 40(5): 475-80, 2002.
Article in English | MEDLINE | ID: mdl-12236260

ABSTRACT

The determination of anisotropy in a phreatic aquifer by means of a pumping test can be carried out, under given conditions, with common analysis methods. This paper develops and applies an amended method based on a technique proposed by Boulton (1970). This new method enables a quick, simple determination of vertical hydraulic conductivity, given drawdown data from a pumping well and at least one observation well, that is applicable to confined phreatic aquifers.


Subject(s)
Fresh Water/chemistry , Geologic Sediments/chemistry , Models, Theoretical , Anisotropy , Water Movements
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