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首页> 外文期刊>Studia Geophysica et Geodaetica >Reflection/transmission laws for slowness vectors in viscoelastic anisotropic media
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Reflection/transmission laws for slowness vectors in viscoelastic anisotropic media

机译:粘弹性各向异性介质中慢度矢量的反射/透射定律

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摘要

The reflection/transmission laws (R/T laws) of plane waves at a plane interface between two homogeneous anisotropic viscoelastic (dissipative) halfspaces are discussed. Algorithms for determining the slowness vectors of reflected/transmitted plane waves from the known slowness vector of the incident wave are proposed. In viscoelastic media, the slowness vectors of plane waves are complex-valued, p = P + iA, where P is the propagation vector, and A the attenuation vector. The proposed algorithms may be applied to bulk plane waves (A = 0), homogeneous plane waves (A ≠ 0, P and A parallel), and inhomogeneous plane waves (A ≠ 0, P and A non-parallel). The manner, in which the slowness vector is specified, plays an important role in the algorithms. For unrestricted anisotropy and viscoelasticity, the algorithms require an algebraic equation of the sixth degree to be solved in each halfspace. The degree of the algebraic equation decreases to four or two for simpler cases (isotropic media, plane waves in symmetry planes of anisotropic media). The physical consequences of the proposed algorithms are discussed in detail.
机译:讨论了平面波在两个均质各向异性粘弹性(耗散)半空间之间的平面界面处的反射/透射定律(R / T律)。提出了从入射波的已知慢度矢量确定反射/透射平面波的慢度矢量的算法。在粘弹性介质中,平面波的慢度矢量是复数值,p = P + iA,其中P是传播矢量,A是衰减矢量。所提出的算法可以应用于体平面波(A = 0),同质平面波(A≠0,P和A平行)和不均匀平面波(A≠0,P和A不平行)。指定慢度矢量的方式在算法中起着重要作用。对于不受限制的各向异性和粘弹性,该算法要求在每个半空间中求解六阶代数方程。对于较简单的情况(各向同性介质,各向异性介质对称平面中的平面波),代数方程的阶数减小为4或2。详细讨论了所提出算法的物理后果。

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