A simple method of obtaining the soil freezing point depression, the unfrozen water content and the pore size distribution curves from the DSC peak maximum temperature-Reference-Cited by-同舟云学术

A simple method of obtaining the soil freezing point depression, the unfrozen water content and the pore size distribution curves from the DSC peak maximum temperature

Published:2016-02 Issue: Volume:122 Page:18-25
ISSN:0165-232X
Container-title:Cold Regions Science and Technology
language:en
Short-container-title:Cold Regions Science and Technology

Author:

Kozlowski Tomasz

Funder

Polish Ministry of Science

Operational Program Human Capital (OP HC)

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences,Geotechnical Engineering and Engineering Geology

Reference31 articles.

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3. The interface between ice and silicate surfaces;Anderson;J. Colloid Interface Sci.,1967

4. Ice nucleation and the substrate–ice interface;Anderson;Nature,1967

5. Low temperature phases of interfacial water in clay–water systems;Anderson;Soil Sci. Soc. Am. Proc.,1971

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