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2—D与3—D横向各向同性介质中地震波动方程的解耦
引用本文:张中杰,何樵登.2—D与3—D横向各向同性介质中地震波动方程的解耦[J].西安石油大学学报(自然科学版),1992(4).
作者姓名:张中杰  何樵登
作者单位:中科院地球物理所,长春地质学院
摘    要:在2-D横向各向同性介质中,似P波与似SV波耦合;3-D介质中,似P波与似SV波及似SH波均耦合于偏微分波动方程组中,为便于2-D与3-D横向各向同性介质中震波激发以及地震记录合成研究,本文首先对波动方程组本身进行了讨论,进而分别研究了二维与三维横向各向同性介质中波动方程组的解耦问题,得到了解耦后的关于位移分量偏微分方程。

关 键 词:二维与三维横向各向同性介质  地震波  偏微分方程组  耦合  解耦

Decoupling of Seismic Motion Equations in 2—D and 3—D Transversely Isotropic Media
Zhang Zhongjie.Decoupling of Seismic Motion Equations in 2—D and 3—D Transversely Isotropic Media[J].Journal of Xian Shiyou University,1992(4).
Authors:Zhang Zhongjie
Abstract:In 2—D TIM (Transversely lsotropic Media), quasi—P wave and quasi—SV were coupled. In 3—D TIM, quasi—P wave, quasi—SV wave and quasi—Sh wave were coupled in partial differential motion equations. For the convenience of studying the seismic record and stimulating seismic wave in 2—D and 3—D TIM, this paper analyses the motion equations first, and then studies the decoupling of seismic motion equations in 2—D and 3—D TIM, respectively, and has obtained the decoupled partial differential equation of displacement component.
Keywords:2—D and 3—D TIM  seismic wave  partial differential equation  coupling  decoupling
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