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Unfrozen water as a function of clay microstructure
Luleå University of Technology, Department of Civil, Environmental and Natural Resources Engineering, Mining and Geotechnical Engineering.ORCID iD: 0000-0002-6851-4839
1979 (English)In: Engineering Geology, ISSN 0013-7952, E-ISSN 1872-6917, Vol. 13, no 1-4, p. 157-162Article in journal (Refereed) Published
Abstract [en]

A previous study of microstructural changes in freezing clay suggested that a ' dispersed ' freshwater clay should have a higher percentage of unfrozen water than a (leached) marine clay with similar mineralogical and granulometrical compositions. This report described an investigation where two such clays were actually compared concerning their contents of unfrozen water. The results confirmed the hypothesis. Thus, the influence of clay microstructure on the amount of unfrozen water was clearly shown. The degree of particle aggregation and the density of the particle aggregates are the main microstructural parameters

Place, publisher, year, edition, pages
1979. Vol. 13, no 1-4, p. 157-162
National Category
Geotechnical Engineering
Research subject
Soil Mechanics
Identifiers
URN: urn:nbn:se:ltu:diva-33230DOI: 10.1016/B978-0-444-41782-4.50018-XScopus ID: 2-s2.0-85023402108Local ID: 80908df0-0ad2-11dd-ae49-000ea68e967bOAI: oai:DiVA.org:ltu-33230DiVA, id: diva2:1006467
Conference
International Conference on Ground Freezing : 08/03/1978 - 10/03/1978
Note

Godkänd; 1979; 20080415 (cira); Konferensartikel i tidskrift

Available from: 2016-09-30 Created: 2016-09-30 Last updated: 2018-06-26Bibliographically approved

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Pusch, Roland

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