Mono-component multiparameter acoustic full waveform inversion in vertically transverse isotropic media using converted vector wavefields
In multiparameter full-waveform inversion (FWI) with acoustic-approximation for vertically transverse isotropic (VTI) media, it is important to choose an appropriate modeling technique for computational efficiency and numerical stability. In addition, because the gradient is determined by the modeli...
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Published in | Journal of applied geophysics Vol. 170; p. 103816 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.11.2019
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Subjects | |
Online Access | Get full text |
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Summary: | In multiparameter full-waveform inversion (FWI) with acoustic-approximation for vertically transverse isotropic (VTI) media, it is important to choose an appropriate modeling technique for computational efficiency and numerical stability. In addition, because the gradient is determined by the modeling algorithm used in the FWI process, we need to examine if the modeling algorithm yields a gradient similar to that obtained from the elastic scattering theory. The decomposed equation with mono-component has been proposed because it is computationally efficient and does not generate shear-wave artifacts. However, the decomposed equation has the limitation that its numerical scattering potentials for the perturbations of anisotropic parameters do not properly simulate the theoretical elastic scattering potentials. To overcome the limitation, we propose using the vector virtual sources to compute the gradient in the FWI algorithm by converting the mono-component (pressure) source and receiver wavefields into the two-component particle displacements using the equation of motion on the staggered grids. Unlike the conventional method, our approach properly simulates PP radiation patterns for anisotropic parameters obtained under the elastic assumption, while retaining computational efficiency achieved by using the mono-component. Numerical examples show that anisotropic parameters are updated in the correct gradient direction by our method in the FWI process.
•The acoustic anisotropic FWI using the pseudo-analytic (mono-component) acoustic wave equation has a difficulty to describe radiation patterns of partial derivative wavefields compare to the elastic scattering theory.•We propose an alternative approach, which calculate the gradient direction with the vector wavefields converted from the mono-component pressure wavefields.•Comparing the scattering pattern of the partial derivative wavefields and sensitivity kernels, we show the vector-based gradient direction from our proposed approach describe the behavior of the partial derivative wavefields in multi-parameter anisotropic FWI.•We verify the accuracy and feasibility of our approach to the simple syncline and the modified Marmosui-2 models. |
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ISSN: | 0926-9851 1879-1859 |
DOI: | 10.1016/j.jappgeo.2019.07.010 |