Moving phreatic surface in a porous slab: An analytical solution

A. R. Kacimov, N. D. Yakimov

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Transient Darcian flow in an inclined rigid fully saturated porous layer is studied. A phreatic surface of fixed shape driven by uniformly increasing (but generally not equal) water levels in the contiguous reservoirs moves upward with a constant velocity. In a system of coordinates travelling with the reservoir water level the real and imaginary parts of the complex potential (an analytic function) and complex coordinate are linearly interconnected along the boundary of the flow domain that allows implementing the Polubarinova-Kochina method. An explicit analytic equation of the free surface is derived and shown to result in non-trivial configurations including the saturated zone overhanging dry areas.

Original languageEnglish
Pages (from-to)399-411
Number of pages13
JournalJournal of Engineering Mathematics
Volume40
Issue number4
DOIs
Publication statusPublished - Aug 2001

Fingerprint

Water levels
Analytical Solution
Water
Complex Potential
Transient Flow
Inclined
Free Surface
Analytic function
Linearly
Configuration

Keywords

  • Complex potential
  • Free surface
  • Hodograph
  • Polubarinova-kochina
  • Porous media

ASJC Scopus subject areas

  • Engineering (miscellaneous)
  • Applied Mathematics

Cite this

Moving phreatic surface in a porous slab : An analytical solution. / Kacimov, A. R.; Yakimov, N. D.

In: Journal of Engineering Mathematics, Vol. 40, No. 4, 08.2001, p. 399-411.

Research output: Contribution to journalArticle

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