Jiandong Huang, Dinghui Yang, Xijun He, Tao Liu, Weijuan Meng
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引用次数: 0
Abstract
The decoupling of P- and S-waves is an essential prerequisite for elastic reverse time migration (RTM), which effectively reduces crosstalk artifacts, but most wavefield separation algorithms are implemented on uniform rectangular grids. We have developed an amplitude- and phase-preserving P- and S-wavefield separation approach on unstructured meshes, which can effectively decompose the original elastic wavefield into P- and S-wavefields. The isotropic case is considered. With the aid of viscoelastic theory, we choose to attenuate P- or S-waves and preserve the other wave mode, so as to achieve wavefield decomposition. Viscoelastic wave equations are first reformulated as decoupling wave equations with a selective strong attenuation. We then use the discontinuous Galerkin (DG) method to simulate decoupling P or S wavefield propagation on triangular and tetrahedral meshes. We adopt a quadrature-free DG approach and the arbitrary mesh is mapped into the reference mesh for numerical calculation, where no additional volume and surface integrations are involved. The amplitude and phase information of this vector decomposition agrees with that of the original elastic data. Four numerical examples are used to demonstrate the superior performance of this vector decomposition algorithm. The isotropic example shows the applicability and correctness of our proposed scheme and the second example displays the superiority in handling strong velocity contrasts. The third example exhibits the mesh flexibility in dealing with complex structures, such as caves, faults, undulating surfaces, etc. The last example shows the effectiveness of our developed algorithm extended to a 3D case.
P 波和 S 波的解耦是弹性反向时间迁移(RTM)的基本前提,可有效减少串扰伪影,但大多数波场分离算法都是在均匀矩形网格上实现的。我们在非结构网格上开发了一种保留振幅和相位的 P 波场和 S 波场分离方法,可有效地将原始弹性波场分解为 P 波场和 S 波场。考虑的是各向同性情况。借助粘弹性理论,我们选择衰减 P 波或 S 波,保留其他波模,从而实现波场分解。粘弹性波方程首先被重新表述为具有选择性强衰减的解耦波方程。然后,我们使用非连续伽勒金(DG)方法模拟解耦 P 或 S 波场在三角形和四面体网格上的传播。我们采用无正交 DG 方法,将任意网格映射到参考网格中进行数值计算,不涉及额外的体积和表面积分。这种矢量分解的振幅和相位信息与原始弹性数据一致。四个数值示例展示了这种矢量分解算法的优越性能。各向同性示例显示了我们提出的方案的适用性和正确性,第二个示例显示了处理强烈速度对比的优越性。第三个例子展示了网格在处理复杂结构(如洞穴、断层、起伏表面等)时的灵活性。最后一个例子展示了我们开发的算法在三维情况下的有效性。
期刊介绍:
Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics.
Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research.
Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring.
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