4.7 Article

Modeling Elastic Wave Propagation Using K-Space Operator-Based Temporal High-Order Staggered-Grid Finite-Difference Method

期刊

出版社

IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/TGRS.2016.2615330

关键词

Extrapolation; finite-difference (FD) method; modeling; seismic waves

资金

  1. 973 Program of China [2013CB228603]
  2. National Science and Technology Program [2016ZX05010-001]
  3. National Natural Science Foundation of China [41174119, 41630314]
  4. Research of Novel Method and Technology of Geophysical Prospecting [CNPC 2016-3302]

向作者/读者索取更多资源

The traditional high-order staggered-grid finite-difference (SGFD) method has high-order accuracy in space, but only the second-order accuracy in time, which makes the traditional SGFD method suffer from a large temporal dispersion error during long-distance wave propagation. This paper develops temporal fourth-and sixth-order and spatial arbitrary even-order SGFD schemes to model isotropic elastic wave propagation. The temporal high-order SGFD schemes have smaller temporal dispersion than the traditional temporal second-order scheme, and thus allow larger time steps to attain a similar accuracy. The developed temporal high-order SGFD schemes are applied to simulate a quasi-stress-velocity wave equation (QWE) that is derived in the framework of a k-space approach. A split QWE (SQWE) is further developed, and numerical simulation of SQWE results in separated P (compressional)-wave and S (shear)-wave. Theoretical computational cost analysis verifies that the numerical simulation of QWE using the temporal fourt-hand sixth-order SGFD schemes is more efficient than the numerical simulation of the traditional stress-velocity wave equation using the traditional temporal second-order SGFD scheme in 2-D. In 3-D, the temporal fourth-order SGFD scheme still runs faster than the traditional temporal second-order scheme; however, the temporal sixth-order scheme is more efficient only when a longer stencil length than 12 is adopted. Numerical examples confirm the correctness of the developed elastic wave modeling schemes.

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