The Water-Ice Phase Composition of Clay/Water Systems. 1. The Kaolinite/Water System.

Previous studies indicated that when water-ice phase composition curves are normalized to unit surface area, the unfrozen water content values at given temperatures for the kaolinite/water system are higher than those of other soils and soil constituents. The water-ice phase composition curve for th...

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Bibliographic Details
Main Authors: Anderson,Duwayne M., Tice,Allen R., Banin,Amos
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1974
Subjects:
Soil Mechanics
Snow
Ice and Permafrost
*Kaolinite
*Clay
*Soils
Water
Ice
Montmorillonite
Freezing
Cold regions
Clay minerals
Clay soils
Frozen soils
permafrost
Online Access:http://www.dtic.mil/docs/citations/AD0782951
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0782951
Description
Summary:Previous studies indicated that when water-ice phase composition curves are normalized to unit surface area, the unfrozen water content values at given temperatures for the kaolinite/water system are higher than those of other soils and soil constituents. The water-ice phase composition curve for this system has been redetermined using an improved isothermal calorimeter and the earlier curve confirmed. (Modified author abstract)

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