Colloid-chemical and mineralogical differences of smectites taken from argillized layers, both from within and outside the slip surfaces in the Kamenose landslide
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Research context
OpenAlex topics: Clay minerals and soil interactions · Soil and Unsaturated Flow · Therapeutic Uses of Natural Elements
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References (13)
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1. Swelling and mineralogy of smectites in paddy soils derived from marine alluvium, Japan10.1016/0016-7061(83)90036-8 ↗
2. Geochemical studies of clay minerals, II. Relation between ionic substitution and swelling in montmorillonites
3. Residual strength of smectite-dominated soils from the Kamenose landslide in Japan10.1139/t87-057 ↗
4. Identification of montmorillonoids10.1111/j.1365-2389.1953.tb00657.x ↗
5. The drained residual strength of cohesive soils10.1680/geot.1981.31.2.181 ↗
6. Particle-particle and particle-water interactions in aqueous clay suspensions, II. Viscosity data and interpretation
7. Forces between clay particles
8. Residual strength of clays in landslide, folded strata and the laboratory10.1680/geot.1985.35.1.3 ↗
9. The Kamenose landslide — the geological background of the Kamenose landslide10.3313/jls1964.18.1 ↗
10. An Introduction to Clay Colloid Chemistry
11. Effects of salt concentration and cation species on the measured cation-exchange capacity of soils and clays
12. Particle-particle and particle-water interactions in aqueous clay suspensions, I. Application of a modified Robinson equation to viscosity data
13. Yamaguchi · 1980 · 44