Step length of full-waveform inversion based on linear search method in multisource domain

Author(s):  
Shoudong Wang ◽  
Jianglong Chen
2019 ◽  
Vol 50 (6) ◽  
pp. 583-599
Author(s):  
Xiaona Ma ◽  
Zhiyuan Li ◽  
Pei Ke ◽  
Shanhui Xu ◽  
Guanghe Liang ◽  
...  

2020 ◽  
Vol 64 (4) ◽  
pp. 483-503
Author(s):  
Xiaona Ma ◽  
Guanghe Liang ◽  
Shanhui Xu ◽  
Zhiyuan Li ◽  
Haixin Feng

Author(s):  
Marcos Bernal-Romero ◽  
Ursula Iturrarán-Viveros

Summary Full-Waveform Inversion (FWI) is a procedure based on the minimization of a misfit (or cost) function applied to the difference between synthetic waveforms and real seismic traces that derives high-resolution velocity models. This is achieved through the iterative adjustment of the velocity model and/or some other physical parameters of the Earth’s subsurface, which generally implies large computational effort. In order to minimize this cost function we explore the use of Adaptive Gradient Optimization (AGO), a variant of Stochastic Gradient Descent (SGD) methods, combining them with a dynamic simultaneous sources strategy that allow us to reduce the computational cost involved in this process. AGO methods are computationally efficient, have little memory requirements and have the capability of adapting the step-length according to the optimization process’ evolution. Since a precise calibration of the step-length is needed to ensure efficiency, the AGOs are well-suited for this task because they are able to adapt the step-length according to the optimization’s development. In this work, we propose a simple non-linear relationship that allows an adjustment of the step-length with respect to the frequencies used in the multiscale FWI, avoiding the line-search strategy’s high computational burden. Additionally, the application of this new step-length rule into the AGO methods with a dynamic simultaneous sources strategy, allow us to concurrently accelerate and significantly improve the FWI’s numerical performance and results. We compare the performance and final results of seven AGO methods, using two different FWI misfit functionals (based on L1 and L2 norms) applied to estimate the final velocity models of two benchmark acoustic models: the Marmousi and the Canadian overthrust BP velocity models.


Geophysics ◽  
2020 ◽  
Vol 86 (1) ◽  
pp. V1-V13 ◽  
Author(s):  
Qinglong He ◽  
Yanfei Wang

Full-waveform inversion (FWI) is a powerful method for providing a high-resolution description of the subsurface. However, the misfit function of the conventional FWI method (metric [Formula: see text]-norm) is usually dominated by spurious local minima owing to its nonlinearity and ill-posedness. In addition, FWI requires intensive wavefield computation to evaluate the gradient and step length. We have considered a general inversion method using a deep neural network (DNN) for the FWI problem. This deep-learning inversion method reparameterizes physical parameters using the weights of a DNN, such that the inversion amounts to reconstructing these weights. One advantage of this deep-learning inversion method is that it can serve as an iterative regularization method, benefiting from the representation of the network. Thus, it is suitable to solve ill-posed nonlinear inverse problems. Furthermore, this method possesses good computational efficiency because it only requires first-order derivatives. In addition, it can easily be accelerated by using multiple graphics processing units and central processing units, for weight updating and forward modeling. Synthetic experiments, based on the Marmousi2, 2004 BP, and a metal ore model, are used to show the numerical performance of the deep-learning inversion method. Comprehensive comparisons with a total-variation regularized FWI are presented to show the ability of our method to recover sharp boundaries. Our numerical results indicate that this deep-learning inversion approach is effective, efficient, and can capture salient features of the model.


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