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Exploration Geophysics Exploration Geophysics Society
Journal of the Australian Society of Exploration Geophysicists
RESEARCH ARTICLE

Multi-parameter full waveform inversion using Poisson’s ratio for elastic media

Ju-Won Oh 1 Dong-Joo Min 2 3
+ Author Affiliations
- Author Affiliations

1 Physical Science and Engineering Division, King Abdullah University of Science and Technology, 4700 Thuwal, 23955-6900, Saudi Arabia.

2 Department of Energy Systems Engineering, Seoul National University, 1 Gwanak-ro, Gwanak-gu, Seoul, 08826, Korea.

3 Corresponding author. Email: spoppy@snu.ac.kr

Exploration Geophysics 48(4) 456-475 https://doi.org/10.1071/EG16063
Submitted: 7 June 2016  Accepted: 8 June 2016   Published: 21 July 2016
Originally submitted to KSEG 16 January 2016, accepted 23 May 2016  

Abstract

In multi-parameter full waveform inversion (FWI), the success of recovering each parameter is dependent on characteristics of the partial derivative wavefields (or virtual sources), which differ according to parameterisation. Elastic FWIs based on the two conventional parameterisations (one uses Lamé constants and density; the other employs P- and S-wave velocities and density) have low resolution of gradients for P-wave velocities (or λ). Limitations occur because the virtual sources for P-wave velocity or λ (one of the Lamé constants) are related only to P–P diffracted waves, and generate isotropic explosions, which reduce the spatial resolution of the FWI for these parameters. To increase the spatial resolution, we propose a new parameterisation using P-wave velocity, Poisson’s ratio, and density for frequency-domain multi-parameter FWI for isotropic elastic media. By introducing Poisson’s ratio instead of S-wave velocity, the virtual source for the P-wave velocity generates P–S and S–S diffracted waves as well as P–P diffracted waves in the partial derivative wavefields for the P-wave velocity. Numerical examples of the cross–triangle–square (CTS) model indicate that the new parameterisation provides highly resolved descent directions for the P-wave velocity. Numerical examples of noise-free and noisy data synthesised for the elastic Marmousi-II model support the fact that the new parameterisation is more robust for noise than the two conventional parameterisations.

Key words: elastic media, frequency domain, full waveform inversion, multi-parameter, parameterisation, Poisson’s ratio, virtual source.


References

Barnes, C., Charara, M., and Tsuchiya, T., 2008, Feasibility study for an anisotropic full waveform inversion of cross-well data: Geophysical Prospecting, 56, 897–906
Feasibility study for an anisotropic full waveform inversion of cross-well data:Crossref | GoogleScholarGoogle Scholar |

Bérenger, 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 |

Choi, Y., Min, D.-J., and Shin, C., 2008, Frequency-domain elastic full waveform inversion using the new pseudo-Hessian matrix: Experience of elastic Marmousi-2 synthetic data: Bulletin of the Seismological Society of America, 98, 2402–2415
Frequency-domain elastic full waveform inversion using the new pseudo-Hessian matrix: Experience of elastic Marmousi-2 synthetic data:Crossref | GoogleScholarGoogle Scholar |

Fletcher, R., and Reeves, C. M., 1964, Function minimization by conjugate gradients: The Computer Journal, 7, 149–154
Function minimization by conjugate gradients:Crossref | GoogleScholarGoogle Scholar |

Gardner, G. H. F., Gardner, L. W., and Gregory, A. R., 1974, Formation velocity and density – the diagnostic basis for stratigraphic traps: Geophysics, 39, 770–780
Formation velocity and density – the diagnostic basis for stratigraphic traps:Crossref | GoogleScholarGoogle Scholar |

Gholami, Y., Brossier, R., Operto, S., Robodetti, A., and Virieux, J., 2013a, Which parameterization is suitable for acoustic vertical transverse isotropic full waveform inversion? Part 1: Sensitivity and trade-off analysis: Geophysics, 78, R81–R105
Which parameterization is suitable for acoustic vertical transverse isotropic full waveform inversion? Part 1: Sensitivity and trade-off analysis:Crossref | GoogleScholarGoogle Scholar |

Gholami, Y., Brossier, R., Operto, S., Robodetti, A., and Virieux, J., 2013b, Which parameterization is suitable for acoustic vertical transverse isotropic full waveform inversion? Part 2: Synthetic and real data case studies from Valhall: Geophysics, 78, R107–R124
Which parameterization is suitable for acoustic vertical transverse isotropic full waveform inversion? Part 2: Synthetic and real data case studies from Valhall:Crossref | GoogleScholarGoogle Scholar |

Ha, T., Chung, W., and Shin, C., 2009, Waveform inversion using a back-propagation algorithm and a Huber function norm: Geophysics, 74, R15–R24
Waveform inversion using a back-propagation algorithm and a Huber function norm:Crossref | GoogleScholarGoogle Scholar |

Jeong, W., Lee, H.-Y., and Min, D.-J., 2012, Full waveform inversion strategy for density in the frequency domain: Geophysical Journal International, 188, 1221–1242
Full waveform inversion strategy for density in the frequency domain:Crossref | GoogleScholarGoogle Scholar |

Köhn, D., Nil, D. D., Kurzmann, A., Przebindowska, A., and Bohlen, T., 2012, On the influence of model parametrization in elastic full waveform tomography: Geophysical Journal International, 191, 325–345
On the influence of model parametrization in elastic full waveform tomography:Crossref | GoogleScholarGoogle Scholar |

Lee, H.-Y., Koo, J. M., Min, D.-J., Kwon, B.-D., and Yoo, H. S., 2010, Frequency-domain elastic full waveform inversion for VTI media: Geophysical Journal International, 183, 884–904
Frequency-domain elastic full waveform inversion for VTI media:Crossref | GoogleScholarGoogle Scholar |

Lines, L. R., and Treitel, S., 1984, Tutorial: A review of least-squares inversion and its application to geophysical problems: Geophysical Prospecting, 32, 159–186
Tutorial: A review of least-squares inversion and its application to geophysical problems:Crossref | GoogleScholarGoogle Scholar |

Mora, P., 1987, Nonlinear two-dimensional elastic inversion of multioffset seismic data: Geophysics, 52, 1211–1228
Nonlinear two-dimensional elastic inversion of multioffset seismic data:Crossref | GoogleScholarGoogle Scholar |

Oh, J.-W., and Min, D.-J., 2013, Weighting technique using back-propagated wavefields incited by deconvolved residuals for frequency-domain elastic waveform inversion: Geophysical Journal International, 194, 322–347
Weighting technique using back-propagated wavefields incited by deconvolved residuals for frequency-domain elastic waveform inversion:Crossref | GoogleScholarGoogle Scholar |

Operto, S. Y., Gholami, Y., Prieux, V., Ribodetti, A., Brossier, R., Métivier, L., and Virieux, J., 2013, A guided tour of multiparameter full-waveform inversion with multicomponent data: From theory to practice: The Leading Edge, 32, 1040–1054
A guided tour of multiparameter full-waveform inversion with multicomponent data: From theory to practice:Crossref | GoogleScholarGoogle Scholar |

Plessix, R.-É., and Cao, Q., 2011, A parametrization study for surface seismic full waveform inversion in an acoustic vertical transversely isotropic medium: Geophysical Journal International, 185, 539–556
A parametrization study for surface seismic full waveform inversion in an acoustic vertical transversely isotropic medium:Crossref | GoogleScholarGoogle Scholar |

Pratt, R. G., Shin, C., and Hicks, G. J., 1998, Gauss-Newton and full Newton methods in frequency-space seismic waveform inversion: Geophysical Journal International, 133, 341–362
Gauss-Newton and full Newton methods in frequency-space seismic waveform inversion:Crossref | GoogleScholarGoogle Scholar |

Prieux, V., Brossier, R., Operto, S., and Virieux, J., 2013a, Multiparameter full waveform inversion of multicomponent ocean-bottom-cable data from the Valhall field. Part 1: imaging compressional wave speed, density and attenuation: Geophysical Journal International, 194, 1640–1664
Multiparameter full waveform inversion of multicomponent ocean-bottom-cable data from the Valhall field. Part 1: imaging compressional wave speed, density and attenuation:Crossref | GoogleScholarGoogle Scholar |

Prieux, V., Brossier, R., Operto, S., and Virieux, J., 2013b, Multiparameter full waveform inversion of multicomponent ocean-bottom-cable data from the Valhall field. Part 2: imaging compressive-wave and shear-wave velocities: Geophysical Journal International, 194, 1665–1681
Multiparameter full waveform inversion of multicomponent ocean-bottom-cable data from the Valhall field. Part 2: imaging compressive-wave and shear-wave velocities:Crossref | GoogleScholarGoogle Scholar |

Tarantola, A., 1986, A strategy for nonlinear elastic inversion of seismic reflection data: Geophysics, 51, 1893–1903
A strategy for nonlinear elastic inversion of seismic reflection data:Crossref | GoogleScholarGoogle Scholar |

Virieux, J., and Operto, S., 2009, An overview of full-waveform inversion in exploration geophysics: Geophysics, 74, WCC1–WCC26
An overview of full-waveform inversion in exploration geophysics:Crossref | GoogleScholarGoogle Scholar |

Zienkiewicz, O. C., and Taylor, R. L., 2000, The finite element method, vol. 1: the basis: Butterworth-Heinemann.