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Pore water expulsion during freezing

Pore water expulsion during freezing

Canadian Geotechnical Journal 12(1): 130-141

ISSN/ISBN: 0008-3674

DOI: 10.1139/t75-012

When a freezing front advances through a saturated soil water may either be expelled or attracted to the freezing front depending upon soil type, stress level, and rate of freezing. Experimental evidence is considered which shows that coarse-grained sandy soils expel water under most conditions while fine grained soils can be made to expel water only at higher overburden pressures.

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Accession: 000462768

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