Heaving Pressure in Soils During Unidirectional Freezing
- 1 November 1967
- journal article
- Published by Canadian Science Publishing in Canadian Geotechnical Journal
- Vol. 4 (4), 398-408
- https://doi.org/10.1139/t67-067
Abstract
Ice lenses in natural soil are normally formed in a thermal gradient regime, and this permits the development of an undulating frost line if a range of pore sizes exists. Evidence is presented that suggests that the undulating nature of the ice-water interface permits the ice lens to form over the smaller pores of the system. Although fractions with only a limited particle size range have been studied, the results support the use of particle size as a valid basis for assessing frost susceptibility.Keywords
This publication has 1 reference indexed in Scilit:
- The thermodynamics of frost damage to porous solidsTransactions of the Faraday Society, 1961