Horizontal infiltration into wet soil

Published

Journal Article

We obtain the long-time asymptotic similarity solution for the wetting front for water absorption from a constant source into a homogenous layer of soil with a preexisting moisture distribution. The presence of the initial water distribution in the soil introduces a time shift that advances the position of the wetting front. The time shift be explicitly calculated for any form of diffusivity. A dynamic time shift is derived to yield a very efficient means for estimating the water content distribution and front position for all times in Brooks-Corey-type soil models.

Full Text

Duke Authors

Cited Authors

  • Witelski, TP

Published Date

  • January 1, 1998

Published In

Volume / Issue

  • 34 / 7

Start / End Page

  • 1859 - 1863

International Standard Serial Number (ISSN)

  • 0043-1397

Digital Object Identifier (DOI)

  • 10.1029/98WR00775

Citation Source

  • Scopus