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Laboratory-determined Phosphorus Flux from Lake Sediments as a Measure of Internal Phosphorus Loading
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Determination of confined phreatic aquifer anisotropy
Carmine Fallico1, Rosa Mazzuca, Salvatore Troisi
1University of Calabria, Department of Soil Conservation, Rende, Cosenza, Italy. fallico@dds.unical.it
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.
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