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A new computer program was developed to simulate vertical compaction in models of regional ground-water flow. The program simulates ground-water storage changes and compaction in discontinuous interbeds or in extensive confining units, accounting for stress-dependent changes in storage properties. The new program is a package for MODFLOW, the U.S. Geological Survey modular finite-difference ground-water flow model. Several features of the program make it useful for application in shallow, unconfined flow systems. Geostatic stress can be treated as a function of water-table elevation, and compaction is a function of computed changes in effective stress at the bottom of a model layer. Thickness of compressible sediments in an unconfined model layer can vary in proportion to saturated thickness.
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Stanley A. Leake
Devin L. Galloway
United States Department of Transportation
Techniques and methods
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Leake et al. (Mon,) studied this question.
synapsesocial.com/papers/6a227e5a39da1a1e72913cdb — DOI: https://doi.org/10.3133/tm6a23