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DC Field | Value | Language |
---|---|---|
dc.contributor.author | Lasani, Zunnoor Ahmed | - |
dc.date.accessioned | 2014-11-07T07:14:23Z | - |
dc.date.accessioned | 2014-11-07T07:15:03Z | - |
dc.date.available | 2014-11-07T07:14:23Z | - |
dc.date.available | 2014-11-07T07:15:03Z | - |
dc.date.issued | 2003 | - |
dc.identifier | M.Tech | en_US |
dc.identifier.uri | http://hdl.handle.net/123456789/7389 | - |
dc.guide | Kashyap, D. | - |
dc.description.abstract | In actual practice most of the water bodies are partially penetrating and as such horizontal flow models are not applicable. In the present study piezometric peak/trough in an aquifer bonded by partially penetrating water bodies is simulated by horizontal flow model employing reduced hydraulic conductivity across the boundary link. A series of numerical experiment were conducted and a relation is evolved which describe the dependence of the ratio of the reduced hydraulic conductivity to the regular hydraulic conductivity on degree of penetration and vertical anisotropy | en_US |
dc.language.iso | en | en_US |
dc.subject | CIVIL ENGINEERING | en_US |
dc.subject | DIRICHLET BOUNDARY CONDITION | en_US |
dc.subject | GROUNDWATER FLOW MODELLING | en_US |
dc.subject | VERTICAL ANISOTROPY | en_US |
dc.title | A STUDY ON DIRICHLET BOUNDARY CONDITION IN GROUNDWATER FLOW MODELLING | en_US |
dc.type | M.Tech Dessertation | en_US |
dc.accession.number | G11210 | en_US |
Appears in Collections: | MASTERS' THESES (Civil Engg) |
Files in This Item:
File | Description | Size | Format | |
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CED G11210.pdf | 1.74 MB | Adobe PDF | View/Open |
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