The technique is designed to measure soil water retention characteristics and to make transient outflow estimates of the soil water diffusivity at temperatures from 5 to 95oC. We also used the technique to determine the isobaric temperature dependence of water retention in soil. Results indicate that at constant capillary pressure, the relationship between moisture content and temperature is hysteretic.-from Authors
Additional publication details
Submersible pressure outflow cell for measurement of soil water retention and diffusivity from 5 to 95oC.