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Phase composition of frozen montmorillonite-water mixtures from heat capacity measurements
Equations and method for determining unfrozen water content of frozen clay-water mixtures from heat capacity measurements; heat capacity of frozen sodium-montmorillonite water mixtures was determined at -4. 7 and -9.6 C with Calve Microcalorimeter; data obtained indicate that method is applicable at temperatures below -5 C; amount of unfrozen water found in frozen clay-water mixtures at -5 to -10 C is equivalent to interfacial surface layer of water of from one to two molecular diameters in thickness; most of this water can be accommodated and is thought to be located in interlamellar regions.
Phase composition of frozen montmorillonite-water mixtures from heat capacity measurements
Equations and method for determining unfrozen water content of frozen clay-water mixtures from heat capacity measurements; heat capacity of frozen sodium-montmorillonite water mixtures was determined at -4. 7 and -9.6 C with Calve Microcalorimeter; data obtained indicate that method is applicable at temperatures below -5 C; amount of unfrozen water found in frozen clay-water mixtures at -5 to -10 C is equivalent to interfacial surface layer of water of from one to two molecular diameters in thickness; most of this water can be accommodated and is thought to be located in interlamellar regions.
Phase composition of frozen montmorillonite-water mixtures from heat capacity measurements
Soil Science Soc America -- Proc
Anderson, D.M. (Autor:in)
1966
6 pages
Aufsatz (Zeitschrift)
Englisch
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