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Formation of Porous Vermiculite Structure in the Course of Swelling

โœ Scribed by L. G. Gordeeva; E. N. Moroz; N. A. Rudina; Yu. I. Aristov

Book ID
110346045
Publisher
SP MAIK Nauka/Interperiodica
Year
2002
Tongue
English
Weight
91 KB
Volume
75
Category
Article
ISSN
1070-4272

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moist porous soil is freezing, a volume expansion is generally observed. The volume increase is mainly due to a water migration process from the base of the soil up to the freezing front, which separates the lower unfrozen part from the upper frozen one. The coupled heat-mass transfer process is acc