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The salinization process of the Israeli Coastal aquifer has led to an average concentration of about 200mgCl/l with a significant number of discrete salinity plumes in the middle and southern regions. The salinity of these plumes is high (500-1000mgCl/l) and is increasing rapidly. Geochemical evidence has suggested that the salinity source in the Be'er Tuvia plume (in the south part of the aquifer)...
It is possible to express the inverse problem for flow in an integral form. The integral formulation affords some insight concerning the recovery of subsurface flow properties. In particular, we find that rapid or high frequency variations in head are primarily sensitive to the specific storage. Conversely, slow or low frequency variations are most strongly influenced by hydraulic conductivity. The...
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