Application of shifted-Laplace preconditioners for heterogenous Helmholtz equation- part 2: Full waveform inversion
Seismic waves bring information from the physical properties of the earth to the surface. Full waveform inversion (FWI) is a local optimization technique which tries to invert the recorded wave fields to the physical properties. An efficient forward-modelling engine along with local differential alg...
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| Format | Journal Article |
| Language | English |
| Published |
23.12.2017
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| Subjects | |
| Online Access | Get full text |
| DOI | 10.48550/arxiv.1712.08743 |
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| Summary: | Seismic waves bring information from the physical properties of the earth to
the surface. Full waveform inversion (FWI) is a local optimization technique
which tries to invert the recorded wave fields to the physical properties. An
efficient forward-modelling engine along with local differential algorithm, to
compute the gradient and Hessian operators, are two key ingredients of FWI
approach. FWI can be done in time or frequency domain. Each method has its own
pros and cons. Here, we only discuss frequency domain method with Krylov
subspace solvers for time-harmonic wave equation. Nonlinearity of the problem
requires good initial macro model of the physical properties and low frequency
data. Macro models are built based on the kinematic information of the recorded
wave fields. Another difficulty is the data modelling algorithm which is hard
to solve especially for high wavenumbers (high frequencies). Without
incorporation of high frequencies in the FWI algorithm we are not going to be
able to update the macro models to high resolution ones. In the companion paper
we showed that efficient forward modelling algorithms can be reached via proper
preconditioners. Here, we will use the preconditioned data modelling engine in
the context of local optimization method to solve for model parameters. The
results show that we yield better convergence of the method and better quality
of the inverted models after using the preconditioned FWI. |
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| DOI: | 10.48550/arxiv.1712.08743 |