MECHANICAL CHARACTERISTICS OF SALT ROCK SUBJECTED TO UNIAXIAL COMPRESSION AND HIGH TEMPERATURE
ZHAI Songtao1,WU Gang2,3,ZHANG Yuan4,WU Xueping1
(1. Department of Civil Engineering,Shanghai Jiao Tong University,Shanghai 200240,China;2. Chinese Underwater Technology Institute,Shanghai Jiao Tong University,Shanghai 200240,China;3. State Key Laboratory for Geomechanics and Deep Underground Engineering,China University of Mining and Technology,Xuzhou,Jiangsu 221008,China;4. Faculty of Architecture and Civil Engineering,Huaiyin Institute of Technology,Huai?an,Jiangsu 223001,China)
Abstract:The uniaxial compression tests for Himalayas salt rock under different temperatures(20 ℃–700 ℃) and after high temperatures(after 100 ℃ and 200 ℃) were conducted to study mechanical characteristics and failure models. The variations of peak stress,peak strain and elastic modulus were analyzed,and especially focusing on the characteristics of stress-strain curves under high temperature. The research results show that,when the temperature is below 120 ℃,the compression strength and elastic modulus of salt rock decrease with temperature increasing,but increase when the temperature changes from 120 ℃ to 200 ℃. Under higher temperatures such as 500 ℃ or above,the internal structure of salt rock changes and the peak stress greatly reduces. The stress-strain curves of salt rock are quite different in different temperature ranges and 170 ℃ is a threshold temperature. When the temperature is 170 ℃–400 ℃,brittle characteristics no longer appears and salt rock shows significant strain hardening with increasing temperature. The limit temperature that Himalayas salt rock can withstand does not exceed 700 ℃. The carrying capacity of samples after high temperature of 100 ℃ and 200 ℃ is relative lower. Simultaneously,its deformation and elastic modulus are lower. There are more cracks and the integrity is inferior.
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ZHAI Songtao1,WU Gang2,3,ZHANG Yuan4,WU Xueping1. MECHANICAL CHARACTERISTICS OF SALT ROCK SUBJECTED TO UNIAXIAL COMPRESSION AND HIGH TEMPERATURE. , 2014, 33(1): 105-111.
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