Abstract
dc:description.abstractThe Porous Medium Equation is a generalization of the Boussinesqequation, when the diffusivity is a power-law function of thehydraulic head, not only a linear function as in the case of theBoussinesq equation. We consider the case of a one-dimensionalaquifer, initially dry, and of semi-infinite extent. At theboundary representing a fluid source, the boundary condition isspecified as a power-law function of time. Following Barenblatt'sapproach, self-similar variables can be introduced. This reducesthe original initial-boundary value problem for the partialdifferential equation to a boundary value problem for a nonlinearordinary differential equation. The boundary representing thewetting front is not known, and must be found in the process ofsolution. A power series solution is found for this nonlinear ODE.We construct a recurrence relation for the coefficients of theseries, and show the convergence of the series. Results arecompared against a highly accurate numerical solution of this ODEas well as the results of a lab-scale experiment.
Degree
thesis:*- Level thesis:degree_level
- Master's Degree
- Year dc:date.issued
- 2012
Author and committee
dc:creator, dc:contributor.*- Author dc:creator
-
- Furtak-Cole, Eden
- Advisor dc:contributor.advisor
-
- Telyakovskiy, Aleksey S.
- Committee members dc:contributor.committeemember
-
- Mortensen, Jeff
- Cooper, Clay
Subjects
dc:subject × 6Rights
dc:rights- Statement dc:rights
-
- In Copyright(All Rights Reserved)
Identifiers
dc:identifier.*- Handle dc:identifier.uri
- http://hdl.handle.net/11714/3679
- OAI identifier oai:identifier
- oai:scholarwolf.unr.edu:11714/3679