单轴应力作用下纵横波的非线性相互作用

Lauren O. Hayes, A. Malcolm, K. Moravej, S. Butt
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引用次数: 3

摘要

裂缝在岩石中的非线性波相互作用中起着重要作用。这些裂缝对于地热能源和非常规油气的开采至关重要,因此了解它们具有重要的实用价值。在这项研究中,我们研究了P波和S波的非线性相互作用作为单轴应力的函数。我们对两个已知有排列裂缝的砂岩样本进行了一组实验,这些砂岩样本取自同一采石场,但经过切割,因此实验的方向与裂缝不同。补充测量表明,速度随应力的增加而减小,表明外加应力打开了两个样品中的裂缝。对于我们的大多数数据,我们观察到非线性响应的显著减少,作为与裂缝方向和实验无关的外加应力的函数。一个有趣的例外是两个s波的耦合,我们观察到非线性响应在较低应力下增加,然后随着载荷的增加而减少。裂缝在岩石中的非线性波相互作用中起着重要作用。这些裂缝对于地热能源和非常规油气的开采至关重要,因此了解它们具有重要的实用价值。在这项研究中,我们研究了P波和S波的非线性相互作用作为单轴应力的函数。我们对两个已知有排列裂缝的砂岩样本进行了一组实验,这些砂岩样本取自同一采石场,但经过切割,因此实验的方向与裂缝不同。补充测量表明,速度随应力的增加而减小,表明外加应力打开了两个样品中的裂缝。对于我们的大多数数据,我们观察到非线性响应的显著减少,作为与裂缝方向和实验无关的外加应力的函数。一个有趣的例外是两个s波的耦合,我们观察到在较低应力下的非线性响应增加。
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Nonlinear interactions of P and S waves under uniaxial stress
Fractures play a significant role in nonlinear wave interactions in rocks. These same fractures are fundamental to the production of geothermal energy as well as unconventional oil and gas, so understanding them has significant practical value. In this study, we examine the nonlinear interactions of P and S waves as a function of uniaxial stress. We perform a set of experiments on two sandstone samples known to have aligned fractures taken from the same quarry but cut so that the experiment is oriented differently with respect to the fractures. Complementary measurements show that the velocity decreases with stress indicating that the applied stress opens the fractures in both samples. For most of our data, we observe a significant decrease in the nonlinear response as a function of the applied stress independent of the orientation of the fractures and the experiment. An interesting exception is the coupling of two S-waves where we observe an increase in the nonlinear response at lower stresses before a decrease as the load is increased.Fractures play a significant role in nonlinear wave interactions in rocks. These same fractures are fundamental to the production of geothermal energy as well as unconventional oil and gas, so understanding them has significant practical value. In this study, we examine the nonlinear interactions of P and S waves as a function of uniaxial stress. We perform a set of experiments on two sandstone samples known to have aligned fractures taken from the same quarry but cut so that the experiment is oriented differently with respect to the fractures. Complementary measurements show that the velocity decreases with stress indicating that the applied stress opens the fractures in both samples. For most of our data, we observe a significant decrease in the nonlinear response as a function of the applied stress independent of the orientation of the fractures and the experiment. An interesting exception is the coupling of two S-waves where we observe an increase in the nonlinear response at lower stresses before a d...
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