分散全波形反演

Ajinkya Kadu, Rajiv Kumar
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引用次数: 3

摘要

随着高效的地震数据采集技术的出现,我们拥有了大量的地震数据,这就提高了全波形反演的地球成像技术。然而,这种反演存在许多问题,包括(i)由于分布式环境中函数和梯度值的重复通信而导致的大量网络等待时间,以及(ii)需要复杂的优化器来解决涉及非光滑正则器的优化问题。为了规避这些问题,我们提出了一种分散的全波形反演方案,该方案在网络中连接的代理在达成共识的同时局部优化其目标。该公式可以用ADMM方法有效地求解。使用标准Marmousi模型证明了该方案可以将正则化与数据拟合解耦,减少网络等待时间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Decentralized Full-Waveform Inversion
With the advent of efficient seismic data acquisition, we are having a surplus of seismic data, which is improving the imaging of the earth using full-waveform inversion. However, such inversion suffers from many issues, including (i) substantial network waiting time due to repeated communications of function and gradient values in the distributed environment, and (ii) requirement of the sophisticated optimizer to solve an optimization problem involving non-smooth regularizers. To circumvent these issues, we propose a decentralized full-waveform inversion, a scheme where connected agents in a network optimize their objectives locally while being in consensus. The proposed formulation can be solved using the ADMM method efficiently. We demonstrate using the standard Marmousi model that such scheme can decouple the regularization from data fitting and reduce the network waiting time.
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