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...
Main Authors: | , , |
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Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1974
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Subjects: | |
Online Access: | http://www.dtic.mil/docs/citations/AD0782951 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0782951 |
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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