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Physical Chemistry of Landslides in Silt and Clay Soils

  • F. Hilbert

Abstract

Basically, there are two different categories of landslides. To the first category belong the slides with purely mechanical causes (e.g., an increase of hydrostatic pressure, erosion, or freezing) without change in the chemical properties of the soil. To the second category belong the slides that are not caused by a change of mechanical forces but by a change in the physical or chemical properties of the soil. Perhaps the most dangerous type of slides occurs because the soil loses its original strength in part (slip surfaces) or as a whole. In extreme cases even a liquefaction may set in and previously solid soils will behave like fluids.

Keywords

Shear Strength Clay Mineral Clay Soil Slip Surface Soil Component 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag New York Inc. 1981

Authors and Affiliations

  • F. Hilbert

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