Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5745
Title: The equation of state of ice and composite frozen soil material
Authors: United States. Advanced Research Projects Agency
Stanford Research Institute
Anderson, Gordon D.
Keywords: Shock waves
Soils
Soil mechanics
Frozen soil
Frozen ground
Ice
Ice crystals
Hugoniot
Equations of state
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.)) ; 257.
Description: Research Report
Abstract: To compute shock wave propagation in frozen soil-water mixtures it is necessary to know a constitutive relation or an equation of state of the medium under consideration. Shock wave techniques provide a powerful tool for the investigation of equations of state at very high stress levels. The stress-volume behavior of frozen soil-water mixtures in the range from 60 to 500 kbar was investigated. Hugoniot data were obtained for Ottawa banding sand (pure quartz sand) and West Lebanon (New Hampshire) glacial till of varying degrees of saturation and for polycrystalline and monocrystalline ice (c-axis oriented in the direction of shock propagation). Release cross curve data were obtained for dry and saturated Ottawa banding sand and for polycrystalline ice. All materials were at an initial temperature of -10°C. In all experiments plane one-dimensional shock waves were used. The Hugoniots and release curves for the soil materials show evidence of a quartz-stishovite phase transition at about 300 kbar. The Hugoniots of single and polycrystalline ice do not differ significantly over the stress range studied - 30 kbar to 300 kbar.
Rights: Approved for public release; distribution is unlimited.
URI: http://hdl.handle.net/11681/5745
Appears in Collections:Research Report

Files in This Item:
File Description SizeFormat 
CRREL-Research-Report-257.pdf12.69 MBAdobe PDFThumbnail
View/Open