Please use this identifier to cite or link to this item: http://dspace.chitkarauniversity.edu.in/xmlui/handle/123456789/468
Full metadata record
DC FieldValueLanguage
dc.contributor.authorPatel, M A-
dc.contributor.authorDesai, N B-
dc.date.accessioned2022-06-07T08:06:06Z-
dc.date.available2022-06-07T08:06:06Z-
dc.date.issued2018-09-06-
dc.identifier.issn2278-9561-
dc.identifier.issn2278-957X-
dc.identifier.urihttp://dspace.chitkarauniversity.edu.in/xmlui/handle/123456789/468-
dc.description.abstractBoussinesq’s equation is one-dimensional nonlinear partial differential equation which represents the infiltration phenomenon. This equation is frequently used to study the infiltration phenomenon in unsaturated porous medium. Infiltration is the process in which the groundwater of the water reservoir has entered in the unsaturated soil through vertical permeable wall. An approximate analytical solution of nonlinear partial differential equation is presented by homotopy analysis method. The convergence of homotopy analysis solution is discussed by choosing proper value of convergence control parameter. The solution represents the height of free surface of infiltrated water.en_US
dc.language.isoenen_US
dc.relation.ispartofseries;CHAENG/2013/49583-
dc.subjectIn iltrationen_US
dc.subjectHomotopy analysis methoden_US
dc.titleHomotopy Analysis Approach of Boussinesq Equation for Infiltration Phenomenon in Unsaturated Porous Medium.en_US
dc.typeArticleen_US
Appears in Collections:Vol. 7 No. 1 (2018)

Files in This Item:
File Description SizeFormat 
11-Article Text-63-1-10-20190523.pdf2.01 MBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.