约束、单轴和纯剪切预应力下弹性波的应力反射和传递

IF 3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Geophysics Pub Date : 2024-05-03 DOI:10.1190/geo2023-0620.1
Haidi Yang, Li-Yun Fu, Tobias M. Müller, Bo-Ye Fu
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引用次数: 0

摘要

对预应力界面上波的反射和透射(R/T)的深入研究在地球物理应用中非常重要,例如利用声波测井数据或地震数据评估随角度变化的弹性特性,以监测地压和构造应力。尽管许多研究都涉及预应力介质中的波传播,但在不同预应力加载模式下,界面上波的随角度变化的 R/T 在很大程度上仍未得到解决。为了解决这个问题,我们运用声弹性理论和三阶声弹性常数来研究两种预应力介质界面处的 R/T 系数。假定应力引起的弹性变形是局部均匀的,没有应力集中引起的边界错位,因此可以应用静态边界条件。我们考虑了三种典型的预应力模式(约束、单轴和纯剪切),每种模式都考虑了上行和下行 P 波和 S 波的发生。推导出不同类型预应力下的诺特方程,然后估算与角度相关的 R/T 系数。界面能量守恒和对预测的 P 波和 S 波模式的声弹性有限差分模拟验证了约束预应力下与角度有关的 R/T 系数的正确性。与弹性情况(预应力 σ=0 兆帕)的比较表明,预应力对反射波和透射波的能量分布具有重要影响,包括与应力相关的临界角、转换波和 R/T 能量比。这种声弹性效应主要发生在临界角前后。对于小角度入射,预应力主要影响 R/T 系数的梯度。预应力的类型和大小与随角度变化的 R/T 系数密切相关,在对预应力介质进行偏移振幅变化分析时必须考虑到这一点。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Stress-dependent reflection and transmission of elastic waves under confining, uniaxial, and pure shear prestresses
Insights into the reflection and transmission (R/T) of waves at a prestressed interface are important in geophysical applications, such as evaluating the angle-dependent elastic properties for monitoring geopressure and tectonic stress using sonic logging data or seismic data. Although many studies deal with wave propagation in prestressed media, the angle-dependent R/T of waves at an interface subject to different prestress loading modes remains largely unaddressed. We address this issue by applying the theory of acoustoelasticity with third-order acoustoelastic constants to study the R/T coefficients at the interface between two prestressed media. Stress-induced elastic deformations are assumed to be locally homogeneous without boundary dislocations caused by stress concentration so that the static boundary conditions can be applied. We consider three typical prestress modes (confining, uniaxial, and pure shear), each of which takes into account the incidence of upgoing and downgoing P and S waves. The Knott equations under different types of prestresses are derived, followed by the estimation of angle-dependent R/T coefficients. The energy conservation at the interface and the acoustoelastic finite-difference simulation of predicted P and S modes verify the correctness of the angle-dependent R/T coefficients under confining prestress. Comparisons with the elastic case (prestress σ=0 MPa) indicate the important influence of prestresses on the energy distribution of reflected and transmitted waves, including stress-dependent critical angles, converted waves, and R/T energy ratios. Such acoustoelastic effects mainly occur around/after the critical angle. For small-angle incidence, prestresses mainly affect the gradient of R/T coefficients. The type and magnitude of prestress are closely related to the angle-dependent R/T coefficients and must be considered for amplitude-variation-with-offset analysis in prestressed media.
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来源期刊
Geophysics
Geophysics 地学-地球化学与地球物理
CiteScore
6.90
自引率
18.20%
发文量
354
审稿时长
3 months
期刊介绍: Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics. Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research. Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring. The PDF format of each Geophysics paper is the official version of record.
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