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Frequency-domain acoustic-wave modeling and inversion of crosshole data: Part Ⅱ—Inversion method, synthetic experiments and real-data results

机译:跨孔数据的频域声波建模与反演:第二部分—反演方法,综合实验与实测结果

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In full-wave inversion of seismic data in complex media it is desirable to use finite differences or finite elements for the forward modeling, but such methods are still prohibitively expensive when implemented in 3-D. Full-wave 2-D inversion schemes are of limited utility even in 2-D media because they do not model 3-D dynamics correctly. Many seismic experiments effectively assume that the geology varies in two dimensions only but generate 3-D (point source) wave-fields; that is, they are "two-and-one-half-dimension-al" (2.5-D), and this configuration can be exploited to model 3-D propagation efficiently in such media. We propose a frequency domain full-wave inversion algorithm which uses a 2.5-D finite difference forward modeling method. The calculated seismogram can be compared directly with real data, which allows the inversion to be iterated. We use a descents-related method to minimize a least-squares measure of the wavefield mismatch at the receivers. The acute non-linearity caused by phase-wrapping, which corresponds to time-domain cycle-skipping, is avoided by the strategy of either starting the inversion using a low frequency component of the data or constructing a starting model using traveltime tomography. The inversion proceeds by stages at successively higher frequencies across the observed bandwidth. The frequency domain is particularly efficient for crosshole configurations and also allows easy incorporation of attenuation, via complex velocities, in both forward modeling and inversion. This also requires the introduction of complex source amplitudes into the inversion as additional unknowns. Synthetic studies show that the iterative scheme enables us to achieve the theoretical maximum resolution for the velocity reconstruction and that strongly attenuative zones can be recovered with reasonable accuracy. Preliminary results from the application of the method to a real data set are also encouraging.
机译:在复杂介质中地震数据的全波反演中,希望对前向建模使用有限差分或有限元,但是当以3-D实施时,此类方法仍然昂贵。即使在2-D媒体中,全波2-D反演方案的实用性也受到限制,因为它们无法正确建模3-D动力学。许多地震实验有效地假设地质学仅在二维上变化,但是会生成3-D(点源)波场;因此,这种方法不会产生任何影响。也就是说,它们是“二维半一维”(2.5-D),并且可以利用此配置来有效建模此类媒体中的3D传播。我们提出一种频域全波反演算法,该算法使用2.5D有限差分正演模拟方法。可以将计算出的地震图直接与真实数据进行比较,从而可以进行反演。我们使用与下降有关的方法来最小化接收器处波场失配的最小二乘法。通过使用数据的低频分量开始反演或使用走时层析成像来构造起始模型的策略,避免了由相位包裹引起的剧烈非线性,这对应于时域循环跳跃。在观察到的带宽内,反演以逐步较高的频率逐步进行。频域对于交叉孔配置特别有效,并且还允许在正演建模和反演中通过复杂的速度轻松合并衰减。这还需要将复杂的源振幅引入反演中,作为其他未知数。综合研究表明,该迭代方案使我们能够实现速度重建的理论最大分辨率,并且可以以合理的精度恢复强衰减区域。该方法应用于真实数据集的初步结果也令人鼓舞。

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