Research Article
Feb 1959
Physico-Chemical Properties of Soils: Soil-Water Systems
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VIEW THE REPLYPublication: Journal of the Soil Mechanics and Foundations Division
Volume 85, Issue 2
Abstract
The heat of wetting, the diffusibility of hydrogen and isotopic prothium-deutrium exchange, indicate that a part of the water in a clay-water system should be considered as belonging to the mineral phase. The minerals thus consist of a central silicate skeleton with an outer part of aqueous composition. The presence of this outer part is the essential characteristic of the mineral phase in a clay-water system. Typical clay properties, such as cohesion and plasticity, are discussed in terms of this concept. The Bowden friction theory is assumed to be valid in clay-water systems.
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Published In
Journal of the Soil Mechanics and Foundations Division
Volume 85 • Issue 2 • February 1959
Pages: 31 - 53
Copyright
© 1959 American Society of Civil Engineers.
History
Published in print: Feb 1959
Published online: Feb 12, 2021
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Authors
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I. Th. Rosenqvist
Prof., Univ. of Oslo, and Head, Geochemical Div., Norwegian Geotechnical Inst., Oslo, Norway
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