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This paper is devoted to a mathematical analysis of some general models of mass transport and other coupled physical processes
developed in simultaneous flows of surface, soil and ground waters. Such models are widely used for forecasting (numerical
simulation) of a hydrological cycle for concrete territories. The mathematical models that proved a more realistic approach
are obtained by combining several mathematical models for local processes. The water-exchange models take into account the
following factors: Water flows in confined and unconfined aquifers, vertical moisture migration allowing earth surface evaporation,
open-channel flow simulated by one-dimensional hydraulic equations, transport of contamination, etc. These models may have
different levels of sophistication. We illustrate the type of mathematical singularities which may appear by considering a
simple model on the coupling of a surface flow of surface and ground waters with the flow of a line channel or river. 相似文献
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Measurement of Ground-Water Parameters Using Salt-Water Injection and Surface Resistivity 总被引:1,自引:0,他引:1
Paul A. White 《Ground water》1988,26(2):179-186
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The Practical Application of Surface Electrical Resistivity to Detection of Ground-Water Pollution 总被引:2,自引:0,他引:2
Daniel W. Urish 《Ground water》1983,21(2):144-152
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Geoelectric Sounding for Delineating Ground-Water Contamination 总被引:1,自引:0,他引:1
William E. Kelly 《Ground water》1976,14(1):6-10
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Statistical Methods for Characterizing Ground-Water Quality 总被引:2,自引:0,他引:2
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Ground-Water Model for a Thick Fresh-Water Lens 总被引:2,自引:0,他引:2
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Abnish C. Amar 《Ground water》1975,13(3):282-292
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