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Investigation of mechanical properties of soft rock due to laboratory reproduction of physical weathering process

机译:实验室对物理风化过程的再现导致的软岩力学特性研究

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摘要

The focus of the present study is on soft rocks (moderately weathered granite and artificial rock) that have suffered physical weathering due to changes in temperature and confining pressure. Unconfined compression tests were conducted on moderately weathered granite, and triaxial compression tests were conducted on artificial rocks. Two test plans were conducted to study the effect of weathering. In the first plan, the specimens suffered weathering process cycles under unconfined conditions, followed by triaxial tests with different confining pressures (0 kPa, 30 kPa, 60 kPa, and 90 kPa). In the second plan, the specimens suffered weathering process cycles under a certain confining pressure (0 kPa, 30 kPa, 60 kPa, and 90 kPa), and the shear strength and initial Young's modulus in each weathering cycle was then studied. Finally, based on the formula of the shear wave velocity and initial Young's modulus, the relationships between normalized shear strength and normalized shear wave velocity were found. These relationships can be used in a further study to understand rock strength on site by detecting the shear wave velocity.
机译:本研究的重点是由于温度和围压变化而遭受物理风化的软岩(中度风化的花岗岩和人造岩)。在中等风化花岗岩上进行无边压缩试验,并在人造岩石上进行三轴压缩试验。进行了两个测试计划以研究风化的影响。在第一个计划中,样品在无限制的条件下经历了风化过程循环,随后进行了三轴试验,采用了不同的围压(0 kPa,30 kPa,60 kPa和90 kPa)。在第二个计划中,样品在一定的围压下(0 kPa,30 kPa,60 kPa和90 kPa)经历了风化过程循环,然后研究了每个风化循环中的剪切强度和初始杨氏模量。最后,根据剪切波速度和初始杨氏模量的公式,得出归一化剪切强度与归一化剪切波速度之间的关系。这些关系可用于进一步的研究中,通过检测剪切波速度来了解现场的岩石强度。

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