Frequency Domain Wave Equation Inversion and Its Application on the Heterogeneous Reservoir Model Data

Zhiyuan Tang
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Abstract

Seismic full waveform inversion seeks to make use of the full information based on full wave field modeling to extract quantitative information from seismograms. Its serious nonlinearity and high dependence on initial velocity model often results in unsatisfactory inversion results in paleo-karsts carbonate reservoir characterized by strong heterogeneity. The paper presents an improved strategy of multi-scale inversion to establish velocity field model of waveform tomography. the forward wave equation algorithm was derived in frequency domain, and then the Matrix formalism for the iterative inverse methods is derived by gradient methods to speed up calculation and to avoid convergence to local minimum value. After massive amount of frequencies tests, the appropriate bandwidth are extracted, and the velocity field calculated at low frequency is used as the input of the high frequency. After the iteration, the accurate velocity field is inverted. Finally, frequency domain wave equation full waveform inversion in mathematical and physical models is conducted in order to verify the inverse program. The method of selecting the inverse frequencies is proved to be effective.
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频域波动方程反演及其在非均质储层模型资料中的应用
地震全波形反演就是利用基于全波场建模的全信息,从地震记录中提取定量信息。对于非均质性强的古岩溶碳酸盐岩储层,其严重的非线性和对初速度模型的高度依赖往往导致反演结果不理想。提出了一种改进的多尺度反演策略,建立了波形层析成像的速度场模型。首先在频域导出了正演波动方程算法,然后利用梯度法导出了迭代反演方法的矩阵形式,以加快计算速度,避免收敛到局部最小值。经过大量的频率测试,提取出合适的带宽,将低频计算得到的速度场作为高频的输入。迭代后,反演出精确的速度场。最后,在数学模型和物理模型中进行频域波动方程全波形反演,以验证反演程序的正确性。结果表明,选择反频率的方法是有效的。
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