Comparison of Soil Freezing Curve and Soil Water Curve Data for Windsor Sandy Loam
Abstract
Unfrozen water content as a function of temperature was measured in the laboratory using nuclear magnetic resonance (NMR) for a Windsor sandy loam soil. The data were related to previously measured soil moisture retention data through the modified Clapeyron equation with suitable adjustment for surface tension. The results show the usefulness of extending the soil freezing curve to temperatures only slightly below freezing and the soil water curve to very great suction.
Document Details
- Document Type
- Technical Report
- Publication Date
- Oct 01, 1988
- Accession Number
- ADA202365
Entities
People
- Allen R. Tice
- Patrick B. Black
Organizations
- Cold Regions Research and Engineering Laboratory