ANALYTIC ELEMENT SOLUTIONS FOR SEEPAGE TOWARDS TOPOGRAPHIC DEPRESSIONS

dc.contributor.authorKacimov A.R.
dc.date.accessioned2024-12-07T09:08:05Z
dc.date.available2024-12-07T09:08:05Z
dc.date.issued2006
dc.description.abstractPoint 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.identifierhttps://www.elibrary.ru/item.asp?id=14684763
dc.identifier.citationJournal of Hydrology, 2006, 318, 1-4, 262-275
dc.identifier.doi10.1016/j.jhydrol.2005.06.019
dc.identifier.issn0022-1694
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46866
dc.subjectANALYTIC SOLUTIONS
dc.subjectEVAPORATION
dc.subjectGROUNDWATER
dc.subjectMOISTURE FLOW
dc.subjectSEEPAGE EROSION
dc.titleANALYTIC ELEMENT SOLUTIONS FOR SEEPAGE TOWARDS TOPOGRAPHIC DEPRESSIONS
dc.typeСтатья

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