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dc.contributor.author Kacimov A.R.
dc.date.accessioned 2024-12-07T09:08:05Z
dc.date.available 2024-12-07T09:08:05Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=14684763
dc.identifier.citation Journal of Hydrology, 2006, 318, 1-4, 262-275
dc.identifier.issn 0022-1694
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46866
dc.description.abstract Point and line singularities are superposed with incident unidirectional saturated and unsaturated flows. The resulting isobars of 3D Laplacian or advective dispersion equation fields model either seepage face dimples and rills on a tilted hillslope or an undulated top of the vadose zone above a stagnant water table. The reconstructed shapes of isobars are conchoidal, i.e. convex-concave. All flow characteristics (drawdowns, velocity and Kirchhoff potential distributions, dimple sizes) are calculated either explicitly or by elementary computer algebra routines. © 2005 Elsevier Ltd All rights reserved.
dc.subject ANALYTIC SOLUTIONS
dc.subject EVAPORATION
dc.subject GROUNDWATER
dc.subject MOISTURE FLOW
dc.subject SEEPAGE EROSION
dc.title ANALYTIC ELEMENT SOLUTIONS FOR SEEPAGE TOWARDS TOPOGRAPHIC DEPRESSIONS
dc.type Статья
dc.identifier.doi 10.1016/j.jhydrol.2005.06.019


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