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Relation between the microfabric of clay soils and their origin and degree of compaction

Osipov, V. I. / Sokolov, V. N.

Summary Results of extensive investigations carried out by the authors on the microstructures of genetic types of clay soils differing in composition, age and degree of compaction are presented. Clays of marine, lacustrine, alluvial, glacial, glacial-lacustrine and eluvial origin have been studied. Investigations were carried out with the help of scanning electron microscopy and the X-ray method. The data obtained have made it possible to ascertain that each genetic type of clay-soil has its characteristic microstructure, which confirms the close interrelation of the microfabric of clay sediments with the conditions of their formation and their subsequent transformation in the course of compaction.

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Relation between the microfabric of clay soils and their origin and degree of compaction

Osipov, V. I. / Sokolov, V. N.

Summary Results of extensive investigations carried out by the authors on the microstructures of genetic types of clay soils differing in composition, age and degree of compaction are presented. Clays of marine, lacustrine, alluvial, glacial, glacial-lacustrine and eluvial origin have been studied. Investigations were carried out with the help of scanning electron microscopy and the X-ray method. The data obtained have made it possible to ascertain that each genetic type of clay-soil has its characteristic microstructure, which confirms the close interrelation of the microfabric of clay sediments with the conditions of their formation and their subsequent transformation in the course of compaction.

Relation between the microfabric of clay soils and their origin and degree of compaction

Osipov, V. I. / Sokolov, V. N.

Summary Results of extensive investigations carried out by the authors on the microstructures of genetic types of clay soils differing in composition, age and degree of compaction are presented. Clays of marine, lacustrine, alluvial, glacial, glacial-lacustrine and eluvial origin have been studied. Investigations were carried out with the help of scanning electron microscopy and the X-ray method. The data obtained have made it possible to ascertain that each genetic type of clay-soil has its characteristic microstructure, which confirms the close interrelation of the microfabric of clay sediments with the conditions of their formation and their subsequent transformation in the course of compaction.

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Title:

Relation between the microfabric of clay soils and their origin and degree of compaction

Contributors:

Osipov, V. I. (author) / Sokolov, V. N. (author)

Published in:

Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur ; 18

Publication date:

1978

ISSN:

DOI:

https://doi.org/10.1007/BF02635351

Type of media:

Article (Journal)

Type of material:

Print

Language:

English

Keywords:

Clay , Glacial Deposit , Compaction , Clay Soil , Bedding Plane

Classification:

BKL: 38.58 Geomechanik / 56.20 Ingenieurgeologie, Bodenmechanik
Local classification TIB: 050/6545

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