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Massively parallel electrical-conductivity imaging of hydrocarbons using the IBM Blue Gene/L supercomputer

机译:使用IBM Blue Gene / L超级计算机对碳氢化合物进行大规模并行电导成像

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Large-scale controlled-source electromagnetic (CSEM) three-dimensional (3D) geophysical imaging is now receiving considerable attention for electrical-conductivity mapping of potential offshore oil and gas reservoirs. To cope with the typically large computational requirements of the 3D CSEM imaging problem, our strategies exploit computational parallelism and optimized finite-difference meshing. We report on an imaging experiment utilizing 32,768 tasks (and processors) on the IBM Blue Gene/L~(TM) (BG/L) supercomputer at the IBM T. J. Watson Research Center. Over a 24-hour period, we were able to image a large-scale marine CSEM field dataset that previously required more than 4 months of computing time on distributed clusters utilizing 1,024 tasks on an InfiniBand? fabric. The total initial data-fitting errors (i.e., "misfits") could be decreased by 67% within 72 completed inversion iterations, indicating the existence of an electrically resistive region in the southern survey area below a depth of 1,500 m underneath the seafloor. The major part of the residual misfit stems from transmitter-parallel receiver components that have an offset from the transmitter sail line (broadside configuration). Modeling confirms that improved broadside data fits can be achieved by considering anisotropic electrical conductivities. While delivering a satisfactory gross-scale image for the depths of interest, the experiment provides important evidence for the necessity of discriminating between horizontal and vertical conductivities for maximally consistent 3D CSEM inversions.
机译:大规模可控源电磁(CSEM)三维(3D)地球物理成像现在正受到潜在海底油气储层电导率测绘的关注。为了应对3D CSEM成像问题的通常较大的计算要求,我们的策略采用了计算并行性和优化的有限差分网格划分。我们报告了在IBM T.J. Watson研究中心的IBM Blue Gene / LTM(BG / L)超级计算机上利用32,768个任务(和处理器)进行的成像实验。在24小时内,我们能够对大型海洋CSEM现场数据集进行成像,该数据集以前需要在InfiniBand?上使用1,024个任务在分布式集群上进行超过4个月的计算时间。布。在72次完整的反演迭代过程中,总的初始数据拟合误差(即“失配”)可以减少67%,这表明南部调查区域在海底下1,500 m深度以下存在电阻区域。残余失配的主要部分是由于与发射器平行的接收器组件(与发射器帆线(宽边配置)有偏移)而引起的。建模证实,考虑到各向异性电导率,可以改善宽边数据拟合度。在为感兴趣的深度提供令人满意的总比例尺图像的同时,该实验为区分最大电导率3D CSEM的水平和垂直电导率提供了重要证据。

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