Standard

3D numerical simulation of elastic waves with a frequency-domain iterative solver. / Belonosov, Mikhail; Kostin, Victor; Neklyudov, Dmitry и др.

в: Geophysics, Том 83, № 6, 01.11.2018, стр. T333-T344.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Belonosov, M, Kostin, V, Neklyudov, D & Tcheverda, V 2018, '3D numerical simulation of elastic waves with a frequency-domain iterative solver', Geophysics, Том. 83, № 6, стр. T333-T344. https://doi.org/10.1190/geo2017-0710.1

APA

Vancouver

Belonosov M, Kostin V, Neklyudov D, Tcheverda V. 3D numerical simulation of elastic waves with a frequency-domain iterative solver. Geophysics. 2018 нояб. 1;83(6):T333-T344. doi: 10.1190/geo2017-0710.1

Author

Belonosov, Mikhail ; Kostin, Victor ; Neklyudov, Dmitry и др. / 3D numerical simulation of elastic waves with a frequency-domain iterative solver. в: Geophysics. 2018 ; Том 83, № 6. стр. T333-T344.

BibTeX

@article{63ea454fb8ff4c7bb9ff3bc55a1fc199,
title = "3D numerical simulation of elastic waves with a frequency-domain iterative solver",
abstract = "The efficiency of any inversion method for estimating the medium parameters from seismic data strongly depends on simulation of the wave propagation, i.e., forward modeling. The requirements are that it should be accurate, fast, and computationally efficient. When the inversion is carried out in the frequency domain (FD), e.g., FD full-waveform inversion, only a few monochromatic components are involved in the computations. In this situation, FD forward modeling is an appealing potential alternative to conventional time-domain solvers. Iterative FD solvers, based on a Krylov subspace iterative method, are of interest due to their moderate memory requirements compared with direct solvers. A huge issue preventing their successful use is a very slow convergence. We have developed an iterative solver for the elastic wave propagation in 3D isotropic heterogeneous land models. Its main ingredient is a novel preconditioner, which provides the convergence of the iteration. We have developed and justified a method to invert our preconditioner effectively on the base of the 2D fast Fourier transform and solving a system of linear algebraic equations with a banded matrix. In addition, we determine how to parallelize our solver using the conventional hybrid parallelization (MPI in conjunction with OpenMP) and demonstrate the good scalability for the widespread 3D SEG/EAGE overthrust model. We find that our method has a high potential for low-frequency simulations in land models with moderate lateral variations and arbitrary vertical variations.",
keywords = "3d, Elastic, Frequency-domain, Modeling, Wave propagation, PROPAGATION",
author = "Mikhail Belonosov and Victor Kostin and Dmitry Neklyudov and Vladimir Tcheverda",
year = "2018",
month = nov,
day = "1",
doi = "10.1190/geo2017-0710.1",
language = "English",
volume = "83",
pages = "T333--T344",
journal = "Geophysics",
issn = "0016-8033",
publisher = "SOC EXPLORATION GEOPHYSICISTS",
number = "6",

}

RIS

TY - JOUR

T1 - 3D numerical simulation of elastic waves with a frequency-domain iterative solver

AU - Belonosov, Mikhail

AU - Kostin, Victor

AU - Neklyudov, Dmitry

AU - Tcheverda, Vladimir

PY - 2018/11/1

Y1 - 2018/11/1

N2 - The efficiency of any inversion method for estimating the medium parameters from seismic data strongly depends on simulation of the wave propagation, i.e., forward modeling. The requirements are that it should be accurate, fast, and computationally efficient. When the inversion is carried out in the frequency domain (FD), e.g., FD full-waveform inversion, only a few monochromatic components are involved in the computations. In this situation, FD forward modeling is an appealing potential alternative to conventional time-domain solvers. Iterative FD solvers, based on a Krylov subspace iterative method, are of interest due to their moderate memory requirements compared with direct solvers. A huge issue preventing their successful use is a very slow convergence. We have developed an iterative solver for the elastic wave propagation in 3D isotropic heterogeneous land models. Its main ingredient is a novel preconditioner, which provides the convergence of the iteration. We have developed and justified a method to invert our preconditioner effectively on the base of the 2D fast Fourier transform and solving a system of linear algebraic equations with a banded matrix. In addition, we determine how to parallelize our solver using the conventional hybrid parallelization (MPI in conjunction with OpenMP) and demonstrate the good scalability for the widespread 3D SEG/EAGE overthrust model. We find that our method has a high potential for low-frequency simulations in land models with moderate lateral variations and arbitrary vertical variations.

AB - The efficiency of any inversion method for estimating the medium parameters from seismic data strongly depends on simulation of the wave propagation, i.e., forward modeling. The requirements are that it should be accurate, fast, and computationally efficient. When the inversion is carried out in the frequency domain (FD), e.g., FD full-waveform inversion, only a few monochromatic components are involved in the computations. In this situation, FD forward modeling is an appealing potential alternative to conventional time-domain solvers. Iterative FD solvers, based on a Krylov subspace iterative method, are of interest due to their moderate memory requirements compared with direct solvers. A huge issue preventing their successful use is a very slow convergence. We have developed an iterative solver for the elastic wave propagation in 3D isotropic heterogeneous land models. Its main ingredient is a novel preconditioner, which provides the convergence of the iteration. We have developed and justified a method to invert our preconditioner effectively on the base of the 2D fast Fourier transform and solving a system of linear algebraic equations with a banded matrix. In addition, we determine how to parallelize our solver using the conventional hybrid parallelization (MPI in conjunction with OpenMP) and demonstrate the good scalability for the widespread 3D SEG/EAGE overthrust model. We find that our method has a high potential for low-frequency simulations in land models with moderate lateral variations and arbitrary vertical variations.

KW - 3d

KW - Elastic

KW - Frequency-domain

KW - Modeling

KW - Wave propagation

KW - PROPAGATION

UR - http://www.scopus.com/inward/record.url?scp=85055497392&partnerID=8YFLogxK

U2 - 10.1190/geo2017-0710.1

DO - 10.1190/geo2017-0710.1

M3 - Article

AN - SCOPUS:85055497392

VL - 83

SP - T333-T344

JO - Geophysics

JF - Geophysics

SN - 0016-8033

IS - 6

ER -

ID: 25774260