DETERMINATION OF DIFFUSIVITY AND HYDRAULIC CONDUCTIVITY IN SOILS AT LOW WATER CONTENTS FROM NONDESTRUCTIVE TRANSIENT FLOW OBSERVATIONS
- 1 January 1986
- journal article
- research article
- Published by Wolters Kluwer Health in Soil Science
- Vol. 141 (1) , 10-19
- https://doi.org/10.1097/00010694-198601000-00003
Abstract
We present an experimental method that nondestructively, relatively quickly, and reproducibly develops data necessary for finite-difference calculations in liqud-vapor diffusivities for water contents between approximately 1% and any intermediate value of interest. Diffusivity functions for five different soils, ranging in texture from fine sands by a clay loam were determined. Vapor absorption and transport mechanisms are discussed in the context of the liquid-vapor diffusivity function, using experimentally measured vapor absorption isotherms. Conductivities calculated from results of experiments conducted using thermocouple psychrometers to nondestructively measure suction heads in a clay loam during the flow process are also presented.Keywords
This publication has 4 references indexed in Scilit:
- Diffusivity and One‐Dimensional Absorption ExperimentsSoil Science Society of America Journal, 1983
- The Soil Water Diffusivity Near SaturationSoil Science Society of America Journal, 1983
- Measurement of Hydraulic Conductivity of Unsaturated Soils with Thermocouple PsychrometersSoil Science Society of America Journal, 1982
- WATER MOVEMENT IN DRY SOILSEuropean Journal of Soil Science, 1968