FRONTAL MOVEMENT OF AQUEOUS SOLUTIONS DURING REDISTRIBUTION THROUGH AIR-DRY SAND COLUMNS AS A FUNCTION OF COLUMN LENGTH AND TIME
- 1 May 1978
- journal article
- research article
- Published by Wolters Kluwer Health in Soil Science
- Vol. 125 (5), 320-325
- https://doi.org/10.1097/00010694-197805000-00008
Abstract
The frontal movement during redistribution of unsorbed waste fronts through an air-dried sand was measured as a function of time and column length for columns from 25-200 cm long. All column data fit an equation of the form S = ETF. S [distance of the wetting front from the soil surface at time T] was found to be significantly correlated with T (at the 1% level). The equation was normalized by dividing S and E [along with F, it is an empirical parameter that must be calculated for each soil] by the column length. When this was done, data for all columns fit a single normalized equation. Use of this equation allows estimation of the shortest possible time necessary for the front of a pulse of waste solution to reach a given depth in a homogeneous soil system.Keywords
This publication has 1 reference indexed in Scilit:
- Ion Distribution, Moisture Content and Density of Soil Columns Measured with Gamma RadiationSoil Science Society of America Journal, 1967