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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Iterative deconvolution and semiblind deconvolution methods in magnetic archaeological prospecting
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Iterative deconvolution and semiblind deconvolution methods in magnetic archaeological prospecting

机译:磁性考古勘探中的迭代反褶积和半盲反褶积方法

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摘要

In archaeological magnetic prospecting, most targets can be modeled by a single layer of constant burial depth and thickness. With this assumption, recovery of the magnetization distribution of the buried layer from magnetic surface measurements is a 2D deconvolution problem. Because this problem is ill posed, it requires regularization techniques to be solved. In analogy with image reconstruction, the solution showing the resolved subsoil features can be considered a focused version of the blurred and noisy magnetic image. Exploiting image deconvolution tools, two iterative reconstruction methods are applied to minimize the least-squares functional: the standard projected Landweber method and a proposed modification of the iterative space reconstruction algorithm. Different regularization functionals inject a priori information in the optimization problem, and the split-gradient method modifies the algorithms. Numerical simulations in the case of perfect knowledge of the impulse response functions demonstrate that the edge-preserving, total-variation functionals give the best results. An iterative semiblind deconvolution method to estimate the burial depth of the source layer was used with a real data set to test the effectiveness of the method.
机译:在考古磁性勘探中,大多数目标可以通过恒定深度的单层埋葬深度和厚度来建模。在此假设下,从磁性表面测量值恢复掩埋层的磁化分布是2D反卷积问题。由于存在此问题,因此需要解决正则化技术。与图像重建类似,可以将显示已解决的地下土壤特征的解决方案视为模糊和嘈杂的磁性图像的聚焦版本。利用图像去卷积工具,应用了两种迭代重建方法以最小化最小二乘函数:标准投影的Landweber方法和对迭代空间重建算法的改进建议。不同的正则化功能会在优化问题中注入先验信息,而拆分梯度方法会修改算法。在完全了解脉冲响应函数的情况下的数值模拟表明,边缘保持,总变化函数可提供最佳结果。使用迭代半盲反卷积方法来估计源层的埋藏深度,并使用真实数据集来测试该方法的有效性。

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