Please use this identifier to cite or link to this item:
http://dspace.chitkarauniversity.edu.in/xmlui/handle/123456789/468
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Patel, M A | - |
dc.contributor.author | Desai, N B | - |
dc.date.accessioned | 2022-06-07T08:06:06Z | - |
dc.date.available | 2022-06-07T08:06:06Z | - |
dc.date.issued | 2018-09-06 | - |
dc.identifier.issn | 2278-9561 | - |
dc.identifier.issn | 2278-957X | - |
dc.identifier.uri | http://dspace.chitkarauniversity.edu.in/xmlui/handle/123456789/468 | - |
dc.description.abstract | Boussinesq’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.iso | en | en_US |
dc.relation.ispartofseries | ;CHAENG/2013/49583 | - |
dc.subject | In iltration | en_US |
dc.subject | Homotopy analysis method | en_US |
dc.title | Homotopy Analysis Approach of Boussinesq Equation for Infiltration Phenomenon in Unsaturated Porous Medium. | en_US |
dc.type | Article | en_US |
Appears in Collections: | Vol. 7 No. 1 (2018) |
Files in This Item:
File | Description | Size | Format | |
---|---|---|---|---|
11-Article Text-63-1-10-20190523.pdf | 2.01 MB | Adobe PDF | View/Open |
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.