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dc.contributor.author | Kacimov A. | |
dc.date.accessioned | 2018-09-17T20:34:41Z | |
dc.date.available | 2018-09-17T20:34:41Z | |
dc.date.issued | 1997 | |
dc.identifier.issn | 0262-6667 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/133700 | |
dc.description.abstract | Transient water table systems under the influence of decaying groundwater mounds are studied in terms of the Dupuit-Forcheimer approximation, its linearization and linear potential theory. Parabolic mounds spreading and shrinking due to gravity and evapotranspiration are derived from the general class defined by Polubarinova-Kochina (1945). The penetration curves are calculated as characteristics of the water table response at prescribed observation wells. The Polubarinova-Kochina solutions for rectangular mounds are used to derive isochrones, a "resting lens" into which a mound transforms, and a distortion picture of reference volumes. These characteristics are obtained from numerical solution of a system of ordinary differential equation. The plume illustrating the advective spread of a contaminant from a reference area is computed as a composition of all path lines passing through this area. | |
dc.relation.ispartofseries | Hydrological Sciences Journal | |
dc.title | Dynamics of groundwater mounds: Analytical solutions and integral characteristics | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 3 | |
dc.relation.ispartofseries-volume | 42 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 329 | |
dc.source.id | SCOPUS02626667-1997-42-3-SID0031156099 |