UNSTEADY FLOW TO BOTTOM DRAIN IN BOUNDED AQUIFER.

Raymond J. Krizek*, Antonio Soriano, Imre Gyuk

*Corresponding author for this work

Research output: Contribution to journalArticle

Abstract

The problem of transient seepage toward a drain at the bottom of a homogeneous, isotropic aquifer is presented. The dependent variables are the position of the free surface, the flow rate, and the pore pressure distributions around the drain, and these are determined as functions of time for various depths of drainage and drain sizes; the characteristics of the aquifer are specified in terms of its coefficient of permeability and its effective porosity.

Original languageEnglish (US)
JournalASCE J Irrig Drain Div
Volume99
Issue numberIR2
StatePublished - Jan 1 1973

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ASJC Scopus subject areas

  • Environmental Science(all)
  • Engineering(all)
  • Earth and Planetary Sciences(all)

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