Conclusions
Based on the principle of freezing point superposition, a model for predicting unfrozen water content is worked out and it can consider the influences of five factors: soil variation, water content, temperature, solution concentration and overburden pressure. The difference of values between determination and calculation is less than 3 %.
According to the curve of unfrozen water content vs. temperature and initial freezing point and temperature at the cold end of soil body, a way for estimating ice segregation temperature is presented. The difference of values between determination and calculation is less than 0.3°C.
The thickness of frozen fringe changing with time has three models. The calculation method needs further study.
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Xu, X., Wang, J., Zhang, L. et al. Mechanism of frost heave by film water migration under temperature gradient. Chin.Sci.Bull. 42, 1290–1294 (1997). https://doi.org/10.1007/BF02882762
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DOI: https://doi.org/10.1007/BF02882762