Please use this identifier to cite or link to this item: http://repository.futminna.edu.ng:8080/jspui/handle/123456789/5735
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dc.contributor.authorShehu, Musa Danjuma-
dc.date.accessioned2021-07-01T11:15:10Z-
dc.date.available2021-07-01T11:15:10Z-
dc.date.issued2017-01-
dc.identifier.citationShehu, M. D., Adeboye K. R. and Ndanusa A. (2017). Finite Element Discretization and Simulation of Groundwater Flow System. Minna Journal of GeoSciences, (MJG), 1(1): 1–10, January.en_US
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/5735-
dc.description.abstractThis paper considered a two dimensional flow in x and y coordinate system and derived a Non-Homogenous Laplace Equation for groundwater flow that is isotropic in nature, using Darcy's equation which for. the basis for the finite element discretization process. By discretizing the Hydraulic Conductivity and Piezometric Head in the x and y direction, a flow direction vector of the groundwater system is obtained.en_US
dc.language.isoenen_US
dc.publisherMinna Journal of Geosciencesen_US
dc.relation.ispartofseries1(1);1-10-
dc.subjectFinite element methoden_US
dc.subjectHydraulic conductivityen_US
dc.subjectGroundwater flowen_US
dc.subjectIsotropic Piezometric headen_US
dc.subjectLaplace equationen_US
dc.titleFinite Element Discretization and Simulation of Groundwater Flow Systemen_US
dc.typeArticleen_US
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