Effect of Exchange Actions on the Frosty Texture of Deposits and the Structure of Segregated Ice

The data received shows that the structure of segregated ice, its crystallographic orientation, as well as the intensity of the ice formation and nature of growth of the ice inclusion, are in direct relationship to the physico-chemical properties of the freezing soil. Three types of frosty texture a...

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Bibliographic Details
Main Author: Konnova,O. S.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1970
Subjects:
Soil Mechanics
Snow
Ice and Permafrost
(*SOILS
FREEZING)
MOISTURE
CRYSTAL GROWTH
SEPARATION
THICKNESS
COLLOIDS
CLAY
SILT
IRON COMPOUNDS
CALCIUM COMPOUNDS
SODIUM COMPOUNDS
POTASSIUM COMPOUNDS
USSR
*FREEZING
*SOILS
TRANSLATIONS
Ice
permafrost
Online Access:http://www.dtic.mil/docs/citations/AD0716595
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0716595
Description
Summary:The data received shows that the structure of segregated ice, its crystallographic orientation, as well as the intensity of the ice formation and nature of growth of the ice inclusion, are in direct relationship to the physico-chemical properties of the freezing soil. Three types of frosty texture and structure of segregated ice have been established in relationship to the physico-chemical properties in freezing soil. (Author) Trans. of Akademiya Nauk SSSR. Institut Merzlotovedeniya. Materialy po Laboratornym Issledovaniyam Merzlykh Gruntov, n4 p53-80 1961.

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