Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5791
Title: Phase composition of pore water in cold rocks
Authors: Mellor, Malcolm.
Keywords: Compressibility
Compressive properties
Electrical conductivity
Electrical resistivity
Phase transformation
Pore water, freezing
Rocks
Rock mechanics
Rock properties
Rock tests
Thermal expansion
Unfrozen water content
Rock moisture
Ice
Issue Date: Dec-1970
Publisher: Cold Regions Research and Engineering Laboratory (U.S.)
Engineer Research and Development Center (U.S.)
Series/Report no.: Research report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 292.
Description: Research Report
Abstract: The phase composition of pore water in three types of rock subjected to temperature below 0°C was explored by a variety of techniques. Freezing point depression was measured as a function of water content by differential thermal analysis, the results yielding relationships between unfrozen water content and temperature. In an effort to avoid the practical difficulties involved in differential thermal analysis, attempts were made to determine freezing characteristics indirectly by air penetration and mercury penetration techniques applied at ordinary room temperatures. Electrical conductivity measurements were made as a function of temperature down to -195° C in an attempt to obtain information on characteristics of interfacial water films at low temperatures. Thermal strain was measured as a function of temperature in order to detect direct mechanical effects associated with phase changes, chiefly strain discontinuities brought about by volume changes in the pore water during rapid freezing and thawing. Finally, isothermal compressibility measurements, with pressures up to 27 kb, were made at - 10°C so as to determine whether the rock underwent step changes in volumetric strain at pressures corresponding to those of the phase boundaries for ice polymorphs.
URI: http://hdl.handle.net/11681/5791
Appears in Collections:CRREL Research Report

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