论文标题

垂直破裂的PP波反射系数:一组对齐裂纹

PP-wave reflection coefficient for vertically cracked media: Single set of aligned cracks

论文作者

Adamus, Filip P.

论文摘要

本文的主要目的是分析裂纹对振幅方位角变化的影响。我们将研究限制为沿水平轴对齐的一组垂直,圆形和平坦的空腔。这些裂纹嵌入各向同性的环境中,或带有垂直对称轴的横向各向同性背景。我们采用有效的培养基理论分别获得具有水平对称轴或正性培养基的横向偏异向物质。为了考虑振幅,我们专注于PP波反射系数的Vavrycuk-Psencik近似。我们假设裂缝位于焊接接触的半空间之一中。方位角变化取决于背景刚度,入射角和裂纹密度参数。通过分析分析,我们指出哪些因素(例如背景的饱和度)导致反射系数在平行或垂直于裂纹方向的方向上具有最大的绝对值。我们讨论了不规则的案例,其中这种极端价值出现在上述方向以外的其他情况下。由于支持数值模拟,我们建议使用方位角进行二维振幅变化的图形模式。模式由一系列形状组成,这些形状随着裂纹密度参数的增加而变化。方案似乎取决于入射角和饱和度。最后,我们提取这些形状,这些形状是含气岩的特征。它们可能被视为气体指示器。我们使用从沉积岩样品中提取的刚度的真实值来支持这些发现并验证我们的模式。

The main goal of this paper is to analyse the influence of cracks on the azimuthal variations of amplitude. We restrict our investigation to a single set of vertical, circular, and flat cavities aligned along a horizontal axis. Such cracks are embedded in either isotropic surroundings or transversely isotropic background with a vertical symmetry axis. We employ the effective medium theory to obtain either transversely-isotropic material with a horizontal symmetry axis or an orthotropic medium, respectively. To consider the amplitudes, we focus on a Vavrycuk-Psencik approximation of the PP-wave reflection coefficient. We assume that cracks are situated in one of the halfspaces being in welded contact. Azimuthal variations depend on the background stiffnesses, incidence angle, and crack density parameter. Upon analytical analysis, we indicate which factors (such as background's saturation) cause the reflection coefficient to have maximum absolute value in the direction parallel or perpendicular to cracks. We discuss the irregular cases, where such extreme values appear in the other than the aforementioned directions. Due to the support of numerical simulations, we propose graphic patterns of two-dimensional amplitude variations with azimuth. The patterns consist of a series of shapes that change with the increasing value of the crack density parameter. Schemes appear to differ depending on the incidence angle and the saturation. Finally, we extract these shapes that are characteristic of gas-bearing rocks. They may be treated as gas indicators. We support the findings and verify our patterns using real values of stiffnesses extracted from the sedimentary rocks' samples.

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