Abstract:Adaptive waveform inversion (AWI) reformulates the misfit function used to perform full-waveform inversion (FWI), so that it no longer contains local minima related to cycle skipping. It does this by finding a model that drives the ratio of the predicted and observed data sets to unity rather than driving the difference between these two data sets to zero as is the case for conventional FWI. We apply AWI to a 3D field data set acquired over a pervasive gas cloud in the North Sea, comparing its performance with… Show more
“…Consequently, solving cycle skipping turns into an important topic in FWI studies. Currently, the first category of proposed methods for cycle skipping is to introduce objective functions that have wider convex region; for example, the objective function based on penalizing the nonzero lags of cross-correlation or deconvolution [e.g., Adaptive Waveform Inversion-AWI (Warner and Guasch 2016;Guasch et al 2019;van Leeuwen and Mulder 2010;Luo and Sava 2011;Zhu and Fomel 2016)], optimal transport distance functions (Métivier et al 2016;, Wavefield Reconstruction Inversion-RWI (van Leeuwen and Herrmann 2013; da Silva and Yao 2017), etc.…”
Full-waveform inversion (FWI) utilizes optimization methods to recover an optimal Earth model to best fit the observed seismic record in a sense of a predefined norm. Since FWI combines mathematic inversion and full-wave equations, it has been recognized as one of the key methods for seismic data imaging and Earth model building in the fields of global/regional and exploration seismology. Unfortunately, conventional FWI fixes background velocity mainly relying on refraction and turning waves that are commonly rich in large offsets. By contrast, reflections in the short offsets mainly contribute to the reconstruction of the high-resolution interfaces. Restricted by acquisition geometries, refractions and turning waves in the record usually have limited penetration depth, which may not reach oil/gas reservoirs. Thus, reflections in the record are the only source that carries the information of these reservoirs. Consequently, it is meaningful to develop reflection-waveform inversion (RWI) that utilizes reflections to recover background velocity including the deep part of the model. This review paper includes: analyzing the weaknesses of FWI when inverting reflections; overviewing the principles of RWI, including separation of the tomography and migration components, the objective functions, constraints; summarizing the current status of the technique of RWI; outlooking the future of RWI.
“…Consequently, solving cycle skipping turns into an important topic in FWI studies. Currently, the first category of proposed methods for cycle skipping is to introduce objective functions that have wider convex region; for example, the objective function based on penalizing the nonzero lags of cross-correlation or deconvolution [e.g., Adaptive Waveform Inversion-AWI (Warner and Guasch 2016;Guasch et al 2019;van Leeuwen and Mulder 2010;Luo and Sava 2011;Zhu and Fomel 2016)], optimal transport distance functions (Métivier et al 2016;, Wavefield Reconstruction Inversion-RWI (van Leeuwen and Herrmann 2013; da Silva and Yao 2017), etc.…”
Full-waveform inversion (FWI) utilizes optimization methods to recover an optimal Earth model to best fit the observed seismic record in a sense of a predefined norm. Since FWI combines mathematic inversion and full-wave equations, it has been recognized as one of the key methods for seismic data imaging and Earth model building in the fields of global/regional and exploration seismology. Unfortunately, conventional FWI fixes background velocity mainly relying on refraction and turning waves that are commonly rich in large offsets. By contrast, reflections in the short offsets mainly contribute to the reconstruction of the high-resolution interfaces. Restricted by acquisition geometries, refractions and turning waves in the record usually have limited penetration depth, which may not reach oil/gas reservoirs. Thus, reflections in the record are the only source that carries the information of these reservoirs. Consequently, it is meaningful to develop reflection-waveform inversion (RWI) that utilizes reflections to recover background velocity including the deep part of the model. This review paper includes: analyzing the weaknesses of FWI when inverting reflections; overviewing the principles of RWI, including separation of the tomography and migration components, the objective functions, constraints; summarizing the current status of the technique of RWI; outlooking the future of RWI.
“…Now the attempt at recovering a reasonable starting model for the skull purely from the data succeeds even though no a-priori model of the skull is assumed. Adaptive waveform inversion has immunity to cycle skipping, which is otherwise a common problem for conventional FWI [27], as well as an increased ability to recover sound-speed information from strong reflections such as those generated by the bones of the skull. We suspect that both of these characteristics may play a role in explaining the improvement of In practice, we suspect that such solutions may not actually be required in a clinical setting, and we have not pursued them further here.…”
Section: Building the Skull Modelmentioning
confidence: 99%
“…Adaptive waveform inversion (AWI) is a form of FWI that has immunity to cycle skipping [26,27]. In conventional FWI, the algorithm seeks to drive the sample-by-sample difference between the predicted and observed data to zero.…”
Section: Adaptive Waveform Inversionmentioning
confidence: 99%
“…Since division in the frequency domain represents deconvolution in the time domain, the AWI algorithm effectively deconvolves one dataset by the other and then attempts to drive the result of that deconvolution towards a unit-amplitude delta function at zero temporal lag. The mathematical details are given on [26], and practical details are given in [27].…”
Magnetic resonance imaging and X-ray computed tomography provide the two principal methods available for imaging the brain at high spatial resolution, but these methods are not easily portable and cannot be applied safely to all patients. Ultrasound imaging is portable and universally safe, but existing modalities cannot image usefully inside the adult human skull. We use in-silico simulations to demonstrate that full-waveform inversion, a computational technique originally developed in geophysics, is able to generate accurate three-dimensional images of the brain with sub-millimetre resolution. This approach overcomes the familiar problems of conventional ultrasound neuroimaging by using: transcranial ultrasound that is not obscured by strong reflections from the skull, low frequencies that are readily transmitted with good signal-to-noise ratio, an accurate wave equation that properly accounts for the physics of wave propagation, and an accurate model of the skull that compensates properly for wavefront distortion. Laboratory ultrasound data, using ex-vivo human skulls, demonstrate that our computational experiments mimic the penetration and signal-to-noise ratios expected in clinical applications. This form of noninvasive neuroimaging has the potential for the rapid diagnosis of stroke and head trauma, and for the provision of routine monitoring of a wide range of neurological conditions.
“…FWI combines this moreaccurate description of the physics with an appropriate non-linear inversion scheme, and a suitable data acquisition geometry, so that it is able to recover fine-scale heterogeneity throughout the model. Adaptive waveform inversion (AWI) 3,19 is a modification of FWI that is better able to begin from a poor starting model; here we use it as a preconditioner for FWI so that inversion can begin successfully without any a priori information about the skull. Figure 1 outlines the geometry of the method.…”
Magnetic resonance imaging and X-ray computed tomography provide the two principal methods available for imaging the brain at high spatial resolution, but these methods are not easily portable and cannot be applied safely to all patients. Ultrasound imaging is portable and universally safe, but existing modalities cannot image usefully inside the adult human skull. We use in silico simulations to demonstrate that full-waveform inversion, a computational technique originally developed in geophysics, is able to generate accurate three-dimensional images of the brain with sub-millimetre resolution. This approach overcomes the familiar problems of conventional ultrasound neuroimaging by using the following: transcranial ultrasound that is not obscured by strong reflections from the skull, low frequencies that are readily transmitted with good signal-to-noise ratio, an accurate wave equation that properly accounts for the physics of wave propagation, and adaptive waveform inversion that is able to create an accurate model of the skull that then compensates properly for wavefront distortion. Laboratory ultrasound data, using ex vivo human skulls and in vivo transcranial signals, demonstrate that our computational experiments mimic the penetration and signal-to-noise ratios expected in clinical applications. This form of non-invasive neuroimaging has the potential for the rapid diagnosis of stroke and head trauma, and for the provision of routine monitoring of a wide range of neurological conditions.
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