Rapid 4D FWI using a local wave solver Abstract Much of the computational cost involved in full-waveform inversion comes from the solution of the wave equation in a large domain. These computations must be done for the entire domain through which we expect waves to pass for a particular survey, despite the fact that our region of interest is often significantly smaller. In addition to the wasted time spent propagating waves through less important parts of the model, computing updates on the entire domain may result in slower convergence of the inversion algorithm due to the larger model space. This can be especially important in 4D seismic monitoring, where we often see the majority of changes within a small subregion of the total domain, such as the reservoir. We present a local wave solver that accurately computes the solution of the wave equation within only a subdomain of the region covered by the survey, representing a significant cost saving in the computation of full-waveform inversion. We also show how this solver can improve the resulting velocity estimates in full-waveform inversion for time-lapse applications and observe that the local solver requires fewer iterations to converge than does the full-domain solver.
IntroductionFull-waveform inversion (FWI) typically involves solving the forward problem of propagating waves from the source to the receiver multiple times per iteration (see, e.g., Virieux and Operto, 2009, and references therein). The calculation of these wavefields is the primary computational cost of an FWI algorithm. However, when waves from the same sources are propagated through a model that has changed little between iterations, much of this computation is repeated from one iteration to the next. For 4D seismic applications, the impact of this repetition on computational cost is greater because we are typically interested in only a small region of the model (e.g., the reservoir), and we may have several data sets to invert. If we are able to perform FWI on only a small subset of the subsurface model, while still taking all of the data into account, we can improve the speed of the inversion process while still preserving the accuracy of the recovered results. To do this, we require an algorithm that solves the wave equation on a subdomain, giving exactly the same wavefield (on that subdomain) as would be obtained when solving the full wave equation in the full domain. We presented such an algorithm in , building upon the work of van Manen et al. (2007). Here, we show how this algorithm can be used to increase the efficiency of FWI for the particular case of 4D velocity change estimation. If there are significant changes outside the reservoir region, as can occur due to compaction for example, then our method may not result in significant cost savings as the number and size of the relevant subdomains grow.Full-waveform inversion for 4D is challenging because of the nonuniqueness of the problem (there are multiple models that fit (Yang et al., 2014a), and model-space regularization me...