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Efficient laplace-domain full waveform inversion using a cyclic shot subsampling method

机译:使用循环散点子采样方法的高效拉普拉斯域全波形反演

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Full waveform inversion is a method used to recover subsurface parameters, and it requires heavy computational resources. We present a cyclic shot subsampling method to make the full waveform inversion efficient while maintaining the quality of the inversion results. The cyclic method subsamples the shots at a regular interval and changes the shot subset at each iteration step. Using this method, we can suppress the aliasing noise present in regular-interval subsampling.We compared the cyclic method with divide-and-conquer, random, and random-in-eachsubgroup subsampling methods using the Laplace-domain full waveform inversion. We found examples of a 2D marine field data set from the Gulf of Mexico and a 3D synthetic salt velocity model. In the inversion examples using the subsampling methods, we could reduce the computation time and obtain results comparable to that without a subsampling technique. The cyclic method and two random subsampling methods yielded similar results; however, the cyclic method generated the best results, especially when the number of shot subsamples was small, as expected. We also examined the effect of subsample updating frequency. The updating frequency does not have a significant effect on the results when the number of subsamples is large. In contrast, frequent subsample updating becomes important when the number of subsamples is small. The random-in-each-subgroup scheme showed the best results if we did not update the subsamples frequently, while the cyclic method suffers from aliasing. The results suggested that the cyclic subsampling scheme can be an alternative to the random schemes and the distributed subsampling schemes with a frequently changing subset are better than lumped subsampling schemes.
机译:全波形反演是一种用于恢复地下参数的方法,它需要大量的计算资源。我们提出一种循环散布子采样方法,以使整个波形反演有效,同时保持反演结果的质量。循环方法以规则的间隔对镜头进行二次采样,并在每个迭代步骤更改镜头子集。使用这种方法,我们可以抑制规则间隔子采样中出现的混叠噪声。我们将循环方法与使用Laplace域全波形反演的分治,随机和每个子组中的子采样方法进行了比较。我们找到了来自墨西哥湾的2D海洋领域数据集和3D合成盐速度模型的示例。在使用子采样方法的反演示例中,我们可以减少计算时间,并获得与没有子采样技术的结果相当的结果。循环法和两种随机二次抽样法产生了相似的结果。但是,循环法产生的结果最好,特别是当散布子样本的数量少时,正如预期的那样。我们还检查了子样本更新频率的影响。当子样本数量很大时,更新频率对结果没有显着影响。相反,当子样本数量少时,频繁的子样本更新变得很重要。如果我们不经常更新子样本,则每个子分组随机方案显示出最好的结果,而循环法则遭受锯齿。结果表明,循环子采样方案可以替代随机方案,并且子集变化频繁的分布式子采样方案要优于集总子采样方案。

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