Deformation of Natural Soil Water Dispersion Systems upon Thawing (Deformatsiya Merzlykh Dispersnykh Gruntov pri Ottaivanii),

Abstract

Dispersed rocks (soils) under natural conditions change their structure during freezing. In rocks there occurs a redistribution of moisture depending on the direction of heat flux with an accumulation of it in places where there is crystallization. In the process of ice liberation there occurs an increase in the total size of the rock, known as 'heaving of rocks during freezing'. The existing idea of frozen rock was reflected in the choice of method for calculating the compaction of frozen rocks during their thawing. (Author)

Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1972
Accession Number
AD0738183

Entities

People

  • F. G. Bakulin
  • V. F. Zhukov

Organizations

  • Cold Regions Research and Engineering Laboratory

Tags

DTIC Thesaurus Topics

  • Crystallization
  • Dispersions
  • Energy
  • Freezing
  • Heat Energy
  • Heat Flux
  • Isothermal Processes
  • Moisture

Readers

  • Geotechnical Engineering.
  • Information Retrieval
  • Thermal Physics or Thermal Science.