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MEASUREMENTS OF COMPRESSIONAL AND SHEAR-WAVE VELOCITIES AT VARIABLE PRESSURE AND TEMPERATURE

机译:在变化的压力和温度下的压缩和剪切波速度的测量

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摘要

Knowledge of compressional and shear-wave velocities can provide important information about the bulk physical properties and composition of the subsurface rocks. Study of the pressure dependence of velocities can be useful to determine the range up-to which velocity can vary, in a particular rock type, as we go down depth. We measured the wave velocities in limestone rock samples, collected from the Rewa (Madhya Pradesh) region of the Vindhyan ranges. Measurements of wave velocities were conducted at variable pressures and temperatures, in a controlled laboratory conditions. Our experiments indicate that there is a decrease in compressional-wave velocity as the pressure increases, whereas shear-wave velocity increases with pressure. P-wave velocities decreases from 5.7 km/s to 5.1 km/s whereas the Shear-wave velocity increases from 2.8 km/s to about 3.15 km/s as we increase the pressure. The pressure dependence of the wave-speeds can be explained to some extent by general closure of the pore-space and cracks in the rock samples.
机译:压缩波和剪切波速度的知识可以提供有关地下岩石的整体物理性质和组成的重要信息。研究速度对压力的依赖关系对于确定特定岩石类型中随着深度下降而可以变化的速度范围很有用。我们测量了从Vindhyan山脉的Rewa(Madhya Pradesh)地区收集的石灰岩样品中的波速。在受控的实验室条件下,在可变压力和温度下进行波速测量。我们的实验表明,随着压力的增加,压缩波的速度会降低,而剪切波的速度会随着压力的增加而增加。随着压力的增加,纵波速度从5.7 km / s降低到5.1 km / s,而横波速度从2.8 km / s增加到约3.15 km / s。波速对压力的依赖性可以在一定程度上解释岩石样品中孔隙和裂缝的普遍闭合。

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