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DC Field | Value | Language |
---|---|---|
dc.contributor.author | Munusamy, Selva Balaji | - |
dc.date.accessioned | 2024-04-25T06:27:29Z | - |
dc.date.available | 2024-04-25T06:27:29Z | - |
dc.date.issued | 2018-10 | - |
dc.identifier.uri | https://link.springer.com/article/10.1007/s10666-018-9636-0 | - |
dc.identifier.uri | http://dspace.bits-pilani.ac.in:8080/jspui/xmlui/handle/123456789/14672 | - |
dc.description.abstract | This paper uses the homotopy perturbation method for the analytical solution of groundwater table fluctuations, in response to the tidal boundary condition, for a coastal unconfined aquifer with sloping beach face. The Boussinesq equation for sloping beach contains two non-linear terms. The governing equation is reconstructed in homotopic form with two virtual perturbation parameters and an auxiliary term. The secular terms generated from the non-linear diffusion term and the slope term are eliminated by using parameter expansions based on two virtual parameters. Two non-dimensional parameters emerge from the solution in the process of eliminating secular terms: (i) parameter equivalent to amplitude parameter and (ii) parameter representing beach slope. The second-order (starting from zeroth-order) solution is presented. The higher-order solution efficiently captures the non-linearity of the problem. | en_US |
dc.language.iso | en | en_US |
dc.publisher | Springer | en_US |
dc.subject | Chemistry | en_US |
dc.subject | Boussinesq Equation | en_US |
dc.subject | Homotopy Perturbation | en_US |
dc.title | On Use of Expanding Parameters and Auxiliary Term in Homotopy Perturbation Method for Boussinesq Equation with Tidal Condition | en_US |
dc.type | Article | en_US |
Appears in Collections: | Department of Civil Engineering |
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