Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5862
Title: Some thermodynamic relationships for soils at or below the freezing point. 2, effects of temperature and pressure on unfrozen soil water
Authors: Low, Philip F.
Anderson, Duwayne M. (Duwayne Marlo), 1927-
Hoekstra, P. (Pieter)
Keywords: Frozen ground
Unfrozen water content
Soils
Frozen soils
Soil water content
Soil freezing
Soil moisture content
Pressure factors
Temperature factors
Thermodynamics
Freezing point depression
Heat capacity
Publisher: Cold Regions Research and Engineering Laboratory (U.S.)
Engineer Research and Development Center (U.S.)
Series/Report no.: Research report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 222 pt.2.
Description: Research Report
Abstract: Thermodynamic methods are presented for calculating, from the water adsorption isotherms, the change in unfrozen water content of a partially frozen soil with temperature at a constant pressure or with pressure at a constant temperature. Then, using pertinent experimental data for Na-Wyoming bentonite, the increase in unfrozen water caused by a confining pressure of 100 atm is obtained as a function of temperature. Such information is shown to be relevant to the mechanical properties of frozen soils under stress.
Rights: Approved for public release; distribution is unlimited.
URI: http://hdl.handle.net/11681/5862
Appears in Collections:Research Report

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