AN INFILTRATION EQUATION WITH PHYSICAL SIGNIFICANCE
- 1 February 1954
- journal article
- research article
- Published by Wolters Kluwer Health in Soil Science
- Vol. 77 (2) , 153-158
- https://doi.org/10.1097/00010694-195402000-00009
Abstract
An approximate equation is developed which relates infiltration to the physical determinants of the system. The equation appears to give quantitative explanation of a number of aspects of infiltration. The partial differential equation describing liquid movement in porous media is generalized and leads to the condition for hydraulic similitude between prototype phenomena and models employing the same medium, but a liquid other than waters.This publication has 3 references indexed in Scilit:
- A NUMERICAL METHOD FOR SOLVING THE FLOW EQUATION FOR WATER IN UNSATURATED MATERIALSSoil Science, 1952
- A TECHNIQUE FOR MEASURING SOIL-MOISTURE TENSIONS IN RAPIDLY CHANGING SYSTEMSSoil Science, 1951
- Antecedent soil moisture and its relation to infiltrationAustralian Journal of Agricultural Research, 1951