Location of singular points in orthorhombic media

IF 0.6 Q4 GEOCHEMISTRY & GEOPHYSICS Geofizicheskiy Zhurnal-Geophysical Journal Pub Date : 2022-08-24 DOI:10.24028/gj.v44i3.261965
Y. Roganov, A. Stovas, V. Roganov
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引用次数: 2

Abstract

The dependence of the location of singular points of orthorhombic (ORT) media on the stiffness coefficients , and phase velocity  at the singularity point is studied under the assumption that  are larger than  and . In this case, singular points appear only at the intersection of slowness surfaces of S1- and S2-waves. To simplify the presentation of the results, the values , are fixed and  changed within the limits at which the stiffness matrix remains positive definite. We define the parameters, , , , which result in 0, 1, or 2 singular points in the symmetry planes of the ORT medium. The types of these singular points and their location on the unit circle are described. It is shown that, by selecting parameters , any singular point in the symmetry plane 13 can be combined with the limiting position of the singularity point in-between the symmetry planes, or this point can be included in the singular curve of the degenerate ORT medium. We derive equations for the semi-axes of an ellipse of conical refraction, which is the image of a singular point from plane 13 in the group domain. Conditions for degeneration of the ellipse of conical refraction into a segment or a point are defined. It is shown that there exists only one ORT medium with a fixed phase velocity  of S1- and S2-waves in a given singular direction n. If we present the ORT media as projections of these vectors n onto the plane 12 and mark the value of the Poincaré index of the S1- or S2-wave at the point n, we get 2 regions with indices 1/2 and –1/2 separated by projection of the singular curve in the form of an ellipse or hyperbola. We compute equations for  of a degenerate ORT medium in terms of the values, , and velocity  of S1-, S2-waves on a singular curve. The singular curve is defined by the intersection of a unit sphere with an elliptic cone. It is proved that a degenerate ORT medium for  or  is, respectively, a transversally isotropic medium with a vertical or horizontal axis of symmetry. The results are illustrated in several examples.
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正交介质中奇异点的定位
在大于和的假设下,研究了正交介质奇异点的位置对奇异点处的刚度系数和相速度的依赖性。在这种情况下,奇异点仅出现在S1波和S2波的慢度表面的相交处。为了简化结果的表示,在刚度矩阵保持正定的极限范围内,值是固定的和变化的。我们定义了参数,在ORT介质的对称平面中产生0、1或2个奇异点。描述了这些奇异点的类型及其在单位圆上的位置。结果表明,通过选择参数,对称平面13中的任何奇异点都可以与对称平面之间奇异点的极限位置相结合,或者该点可以包含在退化ORT介质的奇异曲线中。我们导出了圆锥折射椭圆的半轴方程,该椭圆是群域中平面13的奇异点的图像。定义了圆锥折射椭圆退化为线段或点的条件。结果表明,在给定的奇异方向n上,只有一种具有S1波和S2波的固定相速度的ORT介质。如果我们将ORT介质表示为这些矢量n在平面12上的投影,通过椭圆或双曲线形式的奇异曲线的投影,我们得到了索引为1/2和-1/2的两个区域。我们根据奇异曲线上S1波、S2波的值和速度计算退化ORT介质的方程。奇异曲线是由单位球面与椭圆锥的交点定义的。证明了或的退化ORT介质分别是具有垂直或水平对称轴的横向各向同性介质。通过几个例子说明了结果。
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来源期刊
Geofizicheskiy Zhurnal-Geophysical Journal
Geofizicheskiy Zhurnal-Geophysical Journal GEOCHEMISTRY & GEOPHYSICS-
自引率
60.00%
发文量
50
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