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Multi-scale seismic full waveform inversion in the frequency-domain with a multi-grid method 被引量:2

基于多网格的频率域全波形反演(英文)
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摘要 Although full waveform inversion in the frequency domain can overcome the local minima problem in the time direction, such problem still exists in the space direction because of the media subsurface complexity. Based on the optimal steep descent methods, we present an algorithm which combines the preconditioned bi-conjugated gradient stable method and the multi-grid method to compute the wave propagation and the gradient space. The multiple scale prosperity of the waveform inversion and the multi-grid method can overcome the inverse problems local minima defect and accelerate convergence. The local inhomogeneous three-hole model simulated results and the Marmousi model certify the algorithm effectiveness. 频率域全波形反演虽然克服了时间方向上的局部极小值问题,但是地下介质的复杂性使其在空间域仍然存在局部极小值缺陷。在优化梯度法基础上,本文采用预条件双共轭梯度稳定算法和多重网格方法计算反演中的波场传播和目标函数的梯度,在保证计算速度的同时,减小计算机内存的消耗。频率域波形反演和多重网格的多尺度性质有效改善问题极小值缺陷,加快反演的收敛速度。以局部非均匀的三孔模型和Marmousi模型的数值模拟结果验证了该算法的有效性。
出处 《Applied Geophysics》 SCIE CSCD 2011年第4期303-310,371,共9页 应用地球物理(英文版)
基金 supported by the China State Key Science and Technology Project on Marine Carbonate Reservoir Characterization (No. 2011ZX05004-003) the Basic Research Programs of CNPC during the 12th Five-Year Plan Period (NO.2011A-3603) the Natural Science Foundation of China (No.41104066) the RIPED Young Professional Innovation Fund (NO.2010-13-16-02, 2010-A-26-02)
关键词 Full waveform inversion frequency domain wave equation multi-grid iterative method bi-conjugated gradient stable algorithm 全波形反演 频率域波动方程 多重网格迭代法 双共轭梯度稳定算法
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