Free Standard AU & NZ Shipping For All Book Orders Over $80!
Register      Login
Exploration Geophysics Exploration Geophysics Society
Journal of the Australian Society of Exploration Geophysicists
RESEARCH ARTICLE

Extension of split perfectly matched absorbing layer for 2D wave propagation in porous transversely isotropic media

Jin Qian 1 2 4 Shiguo Wu 1 2 Ruofei Cui 3
+ Author Affiliations
- Author Affiliations

1 Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences, Qingdao, 266071, China.

2 Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China.

3 School of Resource and Geoscience, China University of Mining and Technology, Xuzhou, 221116, China.

4 Corresponding author. Email: qianjin@qdio.ac.cn

Exploration Geophysics 44(1) 25-30 https://doi.org/10.1071/EG12002
Submitted: 9 January 2012  Accepted: 25 September 2012   Published: 13 November 2012

Abstract

The perfectly matched layer (PML) has proven to be efficient in absorbing outgoing waves in elastic and poroelastic media. It has not, however, been applied for porous anisotropic media. We develop the velocity–stress formulation for propagation of seismic waves for fluid-saturated porous anisotropic media with Biot’s equations. Then we extend the split perfectly matched absorbing layer (SPML) to these media and describe the staggered-grid finite-difference scheme. Using fourth-order spatial operators and a second-order temporal operator under 2D Cartesian coordinates, we numerically solve the equations for the solid and fluid particle velocity components, and for the solid stress components and fluid pressure. The energy decay curve we show demonstrates that the algorithm can run stably. Results from the horizontally layered model show that the SPML model absorbs the outgoing wave well, which illustrates the algorithm is efficient for modelling in porous transversely isotropic media.

Key words: modelling, perfectly matched absorbing layer, porous transversely isotropic media, staggered-grid finite-difference.


References

Berenger, J. P., 1994, A perfectly matched layer for the absorption of electromagnetic waves: Journal of Computational Physics, 114, 185–200
A perfectly matched layer for the absorption of electromagnetic waves:Crossref | GoogleScholarGoogle Scholar |

Biot, M. A., 1956, Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-frequency range: The Journal of the Acoustical Society of America, 28, 168–178
Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-frequency range:Crossref | GoogleScholarGoogle Scholar |

Biot, M. A., 1962, Mechanics of deformation and acoustic propagation in porous media: Journal of Applied Physics, 33, 1482–1498
Mechanics of deformation and acoustic propagation in porous media:Crossref | GoogleScholarGoogle Scholar |

Chen, J., 2011, Application of the nearly perfectly matched layer for seismic wave propagation in 2D homogeneous isotropic media: Geophysical Prospecting, 59, 662–672
Application of the nearly perfectly matched layer for seismic wave propagation in 2D homogeneous isotropic media:Crossref | GoogleScholarGoogle Scholar |

Collino, F., and Tsogka, C., 2001, Application of the perfectly matched absorbing layer model to the linear elastodynamic problem in anisotropic heterogeneous media: Geophysics, 66, 294–307

Dai, N., Vafidis, A., and Kanasewich, E. R., 1995, Wave propagation in heterogeneous, porous media: a velocity-stress, finite-difference method: Geophysics, 60, 327–340

Hastings, F. D., Schneider, J. B., and Broschat, S. L., 1996, Application of the perfectly matched layer (PML) absorbing condition to elastic wave propagation: The Journal of the Acoustical Society of America, 100, 3061–3069
Application of the perfectly matched layer (PML) absorbing condition to elastic wave propagation:Crossref | GoogleScholarGoogle Scholar |

Juhlin, C., 1995, Finite-difference elastic wave propagation in 2D heterogeneous transversely isotropic media: Geophysical Prospecting, 43, 843–858
Finite-difference elastic wave propagation in 2D heterogeneous transversely isotropic media:Crossref | GoogleScholarGoogle Scholar |

Kelly, K. R., Ward, R. W., Treitel, S., and Alford, R. M., 1976, Synthetic seismograms: a finite-difference approach: Geophysics, 41, 2–27

Komatitsch, D., and Martin, R., 2007, An unsplit convolutional perfectly matched layer improved at grazing incidence for the seismic wave equation: Geophysics, 72, SM155–SM167

Levander, A. R., 1988, Fourth-order finite-difference P-SV seismograms: Geophysics, 53, 1425–1436

Liu, Y., and Sen, M. K., 2011, 3D acoustic wave modelling with time-space domain dispersion-relation-based finite-difference schemes and hybrid absorbing boundary conditions: Exploration Geophysics, 42, 176–189
3D acoustic wave modelling with time-space domain dispersion-relation-based finite-difference schemes and hybrid absorbing boundary conditions:Crossref | GoogleScholarGoogle Scholar |

Liu, X., Greenhalgh, S., and Zhou, B., 2009, Transient solution for poro-viscoacoustic wave propagation in double porosity media and its limitation: Geophysical Journal International, 178, 375–393
Transient solution for poro-viscoacoustic wave propagation in double porosity media and its limitation:Crossref | GoogleScholarGoogle Scholar |

Liu, X., Greenhalgh, S., and Zhou, B., 2010, Approximating the wave moduli of double porosity media at low frequencies by a single Zener or Kelvin-Voigt element: Geophysical Journal International, 181, 391–398
Approximating the wave moduli of double porosity media at low frequencies by a single Zener or Kelvin-Voigt element:Crossref | GoogleScholarGoogle Scholar |

Liu, X., Greenhalgh, S., and Wang, Y., 2011, 2.5D poroelastic wave modeling in double porosity media: Geophysical Journal International, 186, 1285–1294
2.5D poroelastic wave modeling in double porosity media:Crossref | GoogleScholarGoogle Scholar |

Martin, R., Komatitsch, D., and Ezziani, A., 2008, An unsplit convolutional perfectly matched layer improved at grazing incidence for seismic wave propagation in poroelastic media: Geophysics, 73, T51–T61

Mavko, G., Mukerji, T., and Dvorikin, J., 1998, The rock physics handbook: tools for seismic analysis in porous media: Cambridge University Press.

Qian, J., 2010, Seismic numerical simulation and inversion of fractured coal reservoirs: Ph.D. dissertation, China University of Mining and Technology.

Virieux, J., 1986, P-SV wave propagation in heterogeneous media: velocity-stress finite-difference method: Geophysics, 51, 889–901

Wang, X., Dodds, K., and Zhao, H., 2006, An improved high-order rotated staggered finite-difference algorithm for simulating elastic waves in heterogeneous viscoelastic anisotropic media: Exploration Geophysics, 37, 160–174
An improved high-order rotated staggered finite-difference algorithm for simulating elastic waves in heterogeneous viscoelastic anisotropic media:Crossref | GoogleScholarGoogle Scholar |

Zeng, Y. Q., and Liu, Q. H., 2001, A staggered-grid finite-difference method with perfectly matched layers for poroelastic wave equations: The Journal of the Acoustical Society of America, 109, 2571–2580
A staggered-grid finite-difference method with perfectly matched layers for poroelastic wave equations:Crossref | GoogleScholarGoogle Scholar | 1:STN:280:DC%2BD3MzmsVGhtQ%3D%3D&md5=cd9a1460c9f975b4f4b1530fce03f2a2CAS |

Zeng, Y. Q., He, J. Q., and Liu, Q. H., 2001, The application of the perfectly matched layer in numerical modeling of wave propagation in poroelastic media: Geophysics, 66, 1258–1266