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Full-waveform inversion of GPR data in frequency-domain

机译:GPR数据在频域的全波形反演

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A new full-waveform inversion scheme is developed to obtain high-resolution images of cross-hole ground penetrating radar (GPR) data. The inversion is formulated as a non-linear least squares problem which minimizes errors between synthetic and observed data. The full-waveform modeling is implemented in frequency domain using the finite-difference (FDFD) solution of Maxwell equation. Here, we are using an iterative gradient method (Gauss-Newton) where the gradient is determined by using the forward vector wavefield and the backward-propagated vectorial residual wavefield. The algorithm inverts sequentially from low to high frequencies and permittivity and conductivity distributions can be obtained simultaneously. Preliminary inversion results of a synthetic example for a homogeneous background model with embedded high contrast parameters anomalies show that the permittivity result is comparable with time domain full-waveform inversion that uses an expanding bandwidth for increasing iterations.
机译:开发了一种新的全波形反演方案,以获取跨孔地面穿透雷达(GPR)数据的高分辨率图像。将该反演公式化为非线性最小二乘问题,该问题最小化了合成数据和观测数据之间的误差。使用Maxwell方程的有限差分(FDFD)解决方案在频域中实现全波形建模。在这里,我们使用的是迭代梯度法(Gauss-Newton),其中梯度是通过使用前向矢量波场和后向传播矢量残留波场确定的。该算法从低频到高频依次转换,并且可以同时获得介电常数和电导率分布。具有嵌入式高对比度参数异常的同质背景模型的合成示例的初步反演结果表明,介电常数结果与时域全波形反演可比,后者使用扩展带宽来增加迭代次数。

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