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Influence of Temperature and Water Content on Elastic Properties of Hard Rocks in Thaw/Freeze State Transition

机译:温度和含水量对解冻/冻结状态过渡中硬岩弹性性质的影响

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Elastic properties of enclosing rock mass around Botuobinskaya pipe diamond deposit are studied using the standard STO 05282612-001-2913. The Standard is based on an original procedure for determination of static elastic properties of materials under change in temperature or moisture content, which is inprovided by Russian and international standard but is of practical value in mine planning and design in the permafrost zone. A sample is subjected to multiple loading in the range of low irreversible strains, which improves measurement accuracy and enables physically correct estimation of temperature and water content influence on change of properties in a material in transition from thawed to frozen state. Based on the findings, the mechanisms of change in elastic properties of hard rocks are determined in a wide temperature range. It is emphasized that the change in elastic properties exhibits essentially nonlinear dependence on water content.
机译:使用标准的STO 05282612-001-2913研究了植物宾尼盖管钻矿床附近岩石质量的弹性性质。 该标准基于俄罗斯和国际标准的温度或水分含量变化的静态弹性性能的原始方法,该含水量是永久冻土区矿山规划和设计中的实用价值。 在低不可逆菌株的范围内对样品进行多重载荷,这提高了测量精度,并且可以物理正确地估计温度和水含量对从解冻到冷冻状态的转变中的物质变化的影响。 基于发现,在宽温度范围内确定硬岩弹性性质的变化机制。 强调,弹性物质的变化表现出基本上非线性对水含量的影响。

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