NATURE FLOW OF LANDSLIDES

The article deals with the results obtained by investigating the conditions for the development of flow landslides. Their manifestation is stipulated by the periodical deformation of the structure of water-saturated clayey soil with coagulation contacts between particles. It has been established that the structural deformation of soil is associated with a considerable increase in the pore-water pressure developed in the body of the landslide.

• Corporate Authors:

  International Railway Congress Association

  17-21 rue de Louvrain
  1000 Brussels,   Belgium 
• Authors:
  • Goldstein, M N
  • Turovskaya, A Y
• Publication Date: 1975-1

Media Info

• Features: Figures; References; Tables;
• Pagination: p. 14-18
• Serial:
  • RAIL INTERNATIONAL
  • Volume: 6
  • Issue Number: 1

Subject/Index Terms

• TRT Terms: Clay; Embankments; Geological events; Landslides; Pore water pressures; Soil mechanics; Soil stabilization
• Old TRIS Terms: Embankment stabilization; Geological conditions
• Subject Areas: Geotechnology; Railroads;

Filing Info

• Accession Number: 00095688
• Record Type: Publication
• Source Agency: Rail International
• Files: TRIS
• Created Date: Jul 15 1975 12:00AM