A platform for research: civil engineering, architecture and urbanism
A platform for research: civil engineering, architecture and urbanism
Physico-Chemical Properties of Soils: A Symposium: Mechanical Properties of Soil-Water Systems
The heat of wetting, the diffusibility of hydrogen and isotopic prothiumdeutrium exchange, indicate that a part of the water in a clay-water system should be considered as belonging to the mine ral phase. The minerals thus consist of a central silicate ske leton 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. T ypical clay properties, such as cohesion and plasticity, are described in terms of this concept. The Bowden friction theory is assumed to be valid in clay-water systems.
Physico-Chemical Properties of Soils: A Symposium: Mechanical Properties of Soil-Water Systems
The heat of wetting, the diffusibility of hydrogen and isotopic prothiumdeutrium exchange, indicate that a part of the water in a clay-water system should be considered as belonging to the mine ral phase. The minerals thus consist of a central silicate ske leton 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. T ypical clay properties, such as cohesion and plasticity, are described in terms of this concept. The Bowden friction theory is assumed to be valid in clay-water systems.
Physico-Chemical Properties of Soils: A Symposium: Mechanical Properties of Soil-Water Systems
Rosenqvist, I. Th. (author)
Transactions of the American Society of Civil Engineers ; 126 ; 745-767
2021-01-01
231961-01-01 pages
Article (Journal)
Electronic Resource
Unknown