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Reflection Full Waveform Inversion With Second-Order Optimization Using the Adjoint-State Method
DOI:10.1029/2021JB022135.png)
Abstract
En 中文
In controlled-source seismology, the standard full waveform inversion (FWI) can't reliably recover the macrovelocity structure in the deep part, if the surface seismic data lack of ultra-long offsets and very low frequencies. Reformulating the FWI for pre-critical reflections based on model scale separation leads to reflection waveform inversion (RWI), which aims to improve the reconstruction of low-to-intermediate model wavenumbers. However, the state-of-art RWI approaches rely on the gradient-type optimization, resulting in slow convergence and inaccurate recovery of the deep macrovelocities. Therefore, we present a Hessian-based second-order optimization in the context of RWI. Based on the reflection Frechet derivative with respect to the background model, the approximate Hessian and the point spread functions (PSFs) on toy models with two and three layers are constructed to gain physical insights about parameter coupling and spatial resolution at the scale of low-to-intermediate wavenumbers for finite-offset and band-limited data. The high-velocity anomaly and checkerboard experiments demonstrate the benefit of incorporating the inverse approximate Hessian effect on the functional gradient. Accordingly, for large-scale applications, we propose a matrix-free Gauss-Newton RWI approach, in which the Hessian-vector product is formulated with the second-order adjoint-state method and an optimal updating direction is estimated in the nested inner loop to accelerate the convergence. A synthetic example and an application to the real data from East China Sea demonstrate that the proposed method can improve velocity model building and seismic imaging, especially for the deep targets.
Keywords:
reflection waveform inversion
Hessian
Gauss-Newton
seismic imaging
second-order optimization
Journal
J
IF:
4.1
Papers:
1.4W
Citations:
6.4W
Organization
Cited Papers
The application of an optimal transport to a preconditioned data matching function for robust waveform inversion
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Estimation of elastic constants for HTI media using Gauss-Newton and full-Newton multiparameter full-waveform inversion
GEOPHYSICS
IF3.2
Seismic waveform inversion in the frequency domain, Part 1: Theory and verification in a physical scale model
GEOPHYSICS
IF3.2

