Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5863
Title: Some thermodynamic relationships for soils at or below the freezing point. 1, freezing point depression and heat capacity
Authors: Low, Philip F.
Anderson, Duwayne M. (Duwayne Marlo), 1927-
Hoekstra, P. (Pieter)
Keywords: Soils
Thermal properties
Soil freezing
Soil solutions
Soil solution freezing
Soil moisture content
Frozen ground
Unfrozen water content
Thermodynamics
Water content
Heat capacity
Freezing point depression
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.1.
Description: Research Report
Abstract: An extended equation was derived relating the relative partial molar free energy of water in a soil to its freezing point depression and relative partial molar heat content. The equation was used to prepare a table from which each of these 3 quantities can be ascertained if the other 2 are known. The table was used with experimental data to obtain a curve of freezing point depression vs. water content for Na-Wyoming bentonite. Provided the activity of the liquid water in the clay is a single-valued function of the liquid water content and that the ice has the properties of pure bulk ice, this curve also represents the relationship between freezing point depression and unfrozen water in the partially frozen clay. An equation for the heat capacity of a partially frozen soil was also derived. This equation was employed to calculate the heat capacities of the: clay at different water contents and sub-zero temperatures. A comparison of the calculated unfrozen water contents and heat capacities of the partially frozen Na-Wyoming bentonite with the available experimental data indicated satisfactory agreement, especially as regards the unfrozen water contents.
URI: http://hdl.handle.net/11681/5863
Appears in Collections:CRREL Research Report

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