Existence of a Quasiliquid Film on the Surface of Ice

The hypothesis of existence of a quasiliquid film on the surface of ice at temperatures below its melting point (T(melt)) was first stated by M. Faraday for explanation of a number of mechanical properties of ice. In this report the authors describes the use of nuclear magnetic resonance to discover...

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Bibliographic Details
Main Authors: Kvlividze,V. I., Kiselev,V. F., Ushakova,L. A.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1971
Subjects:
Snow
Ice and Permafrost
Solid State Physics
(*ICE
SURFACE PROPERTIES)
LIQUIDS
FILMS
NUCLEAR MAGNETIC RESONANCE
THICKNESS
CRYSTAL LATTICES
MOBILITY
MOLECULES
USSR
TRANSLATIONS
Faraday
Ice
permafrost
Online Access:http://www.dtic.mil/docs/citations/AD0726864
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0726864
Description
Summary:The hypothesis of existence of a quasiliquid film on the surface of ice at temperatures below its melting point (T(melt)) was first stated by M. Faraday for explanation of a number of mechanical properties of ice. In this report the authors describes the use of nuclear magnetic resonance to discover the nature of the surface of ice. This method makes it possible to obtain the most complete information about the degree of mobility of the molecules. (Author) Trans. of Akademiya Nauk SSSR. Doklady, v191 n5 p1088-1090 1970.

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