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Effect of Temperature on Deformation and failure Behaviors of Inada Granite and Shirahama Sandstone in Water

机译:温度对Inada Granite和Shirahama砂岩在水中变形和失效行为的影响

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摘要

Uniaxial compression test, Brazilian test and fracture toughness test were carried out for Inada granite and Shirahama sandstone in pure water controlling the water temperature between 0 deg C and 80 deg C and the loading rate between 1.67 X 10~(-7) m/s and 5.00 X 10~(-4) m/s The uniaxial compressive strength, Poisson's ratio, Indirect tensile strength and stress intensity factor decreased with the temperature for the both two rocks. This tendency was clearer for Inada granite. Critical compressive strain value (axial strain value at peak load point) of Shirahama sandstone also decreased with temperature. However, the effect of temperature on the critical extensile strain (radial strain at peak load point) was not clear for the both two rocks. Young's modulus seemed to take the peak value at 20 C or 40 deg C. These results were explained based on thermal stress due to anisotropy and difference of thermal expansion coefficient between the mineral crams, stress corrosion and change in viscosity of water.
机译:单轴压缩试验,巴西试验和断裂韧性试验在纯水中进行Inada Granite和Shirahama砂岩,控制水温0℃和80℃之间的水温,装载速率在1.67×10〜(-7)m / s之间和5.00 x 10〜(-4)m / s单轴抗压强度,泊松比,间接拉伸强度和应力强度因子随两个岩石的温度而降低。此趋势更加清晰适用于Inada Granite。 Shirahama砂岩的临界压缩应变值(峰值负载点峰值负载点)也随温度降低。然而,对于两个岩石,温度对临界扩展菌株的影响(峰值负载点处的径向菌株)的影响尚不清楚。杨氏的模量似乎在20℃或40℃下取峰值。由于矿物荷兰,应力腐蚀和水粘度变化的热膨胀系数的各向异性和热膨胀系数的差异,这些结果是基于热应力来解释的。

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