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CORRELATION BETWEEN SEISMIC WAVE VELOCITY, ROCK POROSITY, AND MAXIMUM PRINCIPAL STRESS BASED ON THE LABORATORY TEST DATA

机译:基于实验室测试数据的地震波速度,岩石孔隙度,岩石孔隙度和最大主应力的相关性

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In order to determine the internal relationships among seismic wave velocity, axial pressure, and rock porosity, the rock samples taken from NRS170143 borehole of the Nickel Rim South mine are tested using a Hoek type triaxial cell equipped with axial linear variable differential transducers (LVDTs) and a data acquisition module. The empirical expression between seismic wave velocity and rock pressure is fitted based on the laboratory test data of rock samples. Then, P-V model P- model and (p-s model are createdto analyze the laboratory test data. The results show that: (1) the relationship between axial pressure and rock porosity can be represented by a new empirical equation (p=a*e~b*p-c. With an increase of axial pressure, the value of rock porosity gradually decreases below the straight line q>=l% and close to 0.
机译:为了确定地震波速度,轴向压力和岩石孔隙率之间的内部关系,使用配备有轴向线性可变差分传感器(LVDT)的Hoek型三轴电池来测试从NRS170143镍钻镍钻孔的岩石样品 和数据采集模块。 基于岩石样品的实验室测试数据,抗震波速度和岩石压力之间的经验表达。 然后,PV模型P- l%并接近0。

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