起伏海底界面上覆液相弹性介质的海底电缆数据正演模拟与波形分离方法(英文)
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  • 英文篇名:Forward modeling of ocean-bottom cable data and wave-mode separation in fluid–solid elastic media with irregular seabed
  • 作者:曲英铭 ; 孙军治 ; 李振春 ; 黄建平 ; 李海鹏 ; 孙文之
  • 英文作者:Qu Ying-Ming;Sun Jun-Zhi;Li Zhen-Chun;Huang Jian-Ping;Li Hai-Peng;Sun Wen-Zhi;Department of Geophysics, School of Geosciences, China University of Petroleum;SINOPEC Key Laboratory of Geophysics;
  • 关键词:起伏海底界面 ; 上覆液相弹性介质 ; 海底电缆数据 ; 纵横波分离 ; 曲坐标系
  • 英文关键词:Irregular seabed;;fluid-solid elastic media;;ocean bottom cable data;;P- and S-wave separation;;curvilinear coordinates
  • 中文刊名:CAGJ
  • 英文刊名:应用地球物理(英文版)
  • 机构:中国石油大学(华东)地球科学与技术学院;中国石化地球物理重点实验室;
  • 出版日期:2018-12-15
  • 出版单位:Applied Geophysics
  • 年:2018
  • 期:v.15
  • 基金:financially supported by the Natural Science Foundation of China(No.41774133);; the Open Funds of SINOPEC Key Laboratory of Geophysics(No.wtyjy-wx2017-01-04);; National Science and Technology Major Project of the Ministry of Science and Technology of China(No.2016ZX05024-003-011)
  • 语种:英文;
  • 页:CAGJ2018Z1007
  • 页数:18
  • CN:Z1
  • ISSN:11-5212/O
  • 分类号:70-85+205-206
摘要
在海洋地震勘探中,海底电缆技术能够准确记录多分量地震波场。但地震波在海洋上覆液相弹性介质环境中的传播无法用单一的波动方程进行稳定地模拟,而且当海底界面为起伏构造时,常规有限差分格式无法准确地对声波波场传递到弹性波波场的过程进行模拟。因此,提出了一种曲坐标系下的声弹耦合方程正演模拟及纵横波矢量分解方法。该方法将起伏海底界面的上覆液相弹性介质剖分为正交曲网格,并采用坐标旋转将笛卡尔坐标系下的起伏海底界面映射为曲坐标系下的水平海底界面,在上覆液相介质和下伏固相介质中分别采用曲坐标系下的声波方程和弹性波方程进行模拟,在起伏海底界面处,提出了一种曲坐标系下的声-弹耦合控制方程将两种方程的声压和应力结合起来。在数值离散时,引入了一种全交错网格机制提高数值模拟的稳定性。基于上述研究,推导了一种曲坐标系下分离的纵波方程和横波方程,实现了曲坐标系下纵横波矢量分解。分别采用理论推导和数值测试证明了该方法的正确性。
        In marine seismic exploration, ocean-bottom cable techniques accurately record the multicomponent seismic wavefield; however, the seismic wave propagation in fluid–solid media cannot be simulated by a single wave equation. In addition, when the seabed interface is irregular, traditional finite-difference schemes cannot simulate the seismic wave propagation across the irregular seabed interface. Therefore, an acoustic–elastic forward modeling and vector-based P-and S-wave separation method is proposed. In this method, we divide the fluid–solid elastic media with irregular interface into orthogonal grids and map the irregular interface in the Cartesian coordinates system into a horizontal interface in the curvilinear coordinates system of the computational domain using coordinates transformation. The acoustic and elastic wave equations in the curvilinear coordinates system are applied to the fluid and solid medium, respectively. At the irregular interface, the two equations are combined into an acoustic–elastic equation in the curvilinear coordinates system. We next introduce a full staggered-grid scheme to improve the stability of the numerical simulation. Thus, separate P-and S-wave equations in the curvilinear coordinates system are derived to realize the P-and S-wave separation method.
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