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Reducing disk storage of full-3D seismic waveform tomography (F3DT) through lossy online compression

机译:通过有损在线压缩减少全3D地震波形层析成像(F3DT)的磁盘存储

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Full-3D seismic waveform tomography (F3DT) is the latest seismic tomography technique that can assimilate broadband, multi-component seismic waveform observations into high-resolution 3D subsurface seismic structure models. The main drawback in the current F3DT implementation, in particular the scattering-integral implementation (F3DT-SI), is the high disk storage cost and the associated I/O overhead of archiving the 4D space-time wavefields of the receiver- or source-side strain tensors. The strain tensor fields are needed for computing the data sensitivity kernels, which are used for constructing the Jacobian matrix in the Gauss-Newton optimization algorithm. In this study, we have successfully integrated a lossy compression algorithm into our F3DT-SI workflow to significantly reduce the disk space for storing the strain tensor fields. The compressor supports a user-specified tolerance for bounding the error, and can be integrated into our finite-difference wave-propagation simulation code used for computing the strain fields. The decompressor can be integrated into the kernel calculation code that reads the strain fields from the disk and compute the data sensitivity kernels. During the wave-propagation simulations, we compress the strain fields before writing them to the disk. To compute the data sensitivity kernels, we read the compressed strain fields from the disk and decompress them before using them in kernel calculations. Experiments using a realistic dataset in our California statewide F3DT project have shown that we can reduce the strain-field disk storage by at least an order of magnitude with acceptable loss, and also improve the overall I/O performance of the entire F3DT-SI workflow significantly. The integration of the lossy online compressor may potentially open up the possibilities of the wide adoption of F3DT-SI in routine seismic tomography practices in the near future. (C) 2016 Elsevier Ltd. All rights reserved.
机译:全3D地震波形层析成像(F3DT)是最新的地震层析成像技术,可以将宽带,多分量地震波形观测吸收到高分辨率3D地下地震构造模型中。当前F3DT实现方式(尤其是散射积分实现方式(F3DT-SI))的主要缺点是磁盘存储成本高以及归档接收方或源方4D空时波场的相关I / O开销。侧应变张量。计算数据敏感度内核需要应变张量场,该数据用于在高斯-牛顿优化算法中构造雅可比矩阵。在这项研究中,我们已经成功地将有损压缩算法集成到F3DT-SI工作流程中,以显着减少用于存储应变张量场的磁盘空间。该压缩器支持用户指定的误差限制公差,并且可以集成到我们的用于计算应变场的有限差分波传播仿真代码中。可以将解压缩器集成到内核计算代码中,该代码从磁盘读取应变场并计算数据敏感性内核。在波传播模拟过程中,我们先将应变场压缩,然后再将其写入磁盘。为了计算数据敏感性内核,我们在磁盘计算中使用压缩应变场之前先将其压缩并解压缩。在加利福尼亚州全州F3DT项目中使用实际数据集进行的实验表明,我们可以将应变场磁盘存储量减少至少一个数量级,并且可接受的损耗,还可以改善整个F3DT-SI工作流程的总体I / O性能显着。有损在线压缩机的集成可能会在不久的将来开辟F3DT-SI在常规地震层析成像实践中广泛采用的可能性。 (C)2016 Elsevier Ltd.保留所有权利。

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