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Variation in the density of clay minerals with a crystal lattice that swells during hydration is examined. It is demonstrated that greatest intracrystal swelling is attained at the maximum hygroscopic moisture content, involving a reduction to 49% in the density of the solid component. The concept of intracrystal ultramicroporosity ns is introduced. The values of ns, which must be considered for solution of practical problems, is analyzed.
Variation in the density of clay minerals with a crystal lattice that swells during hydration is examined. It is demonstrated that greatest intracrystal swelling is attained at the maximum hygroscopic moisture content, involving a reduction to 49% in the density of the solid component. The concept of intracrystal ultramicroporosity ns is introduced. The values of ns, which must be considered for solution of practical problems, is analyzed.
Density of clay minerals
Osipov, V. I. (author)
2012
Article (Journal)
Electronic Resource
English
BKL:
56.20
Ingenieurgeologie, Bodenmechanik
/
56.20$jIngenieurgeologie$jBodenmechanik
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