从一维正演Aem反演模型定量评价可解释带

W. Deleersnyder, D. Dudal, T. Hermans, K. Leuven, Kulak
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引用次数: 0

摘要

全三维反演时域AEM数据需要专家的专业知识和大量的计算资源,并不是每个人都能轻易获得。因此,准2d /3D反演方法盛行,使用更快但近似的(1D)正演模型。问题是所得的反演结果是否可靠,能否定量解释。我们提出了一种准2D/3D方法的评估工具,该工具可以指示反演模型中与多维(2D/3D)正演模型不一致的区域,因此不应以定量方式进行解释。图像评估步骤只需要一个完整的2.5D或3D正演和一个多维雅可比计算在粗网格上计算所谓的归一化梯度。该梯度的大值表明模型参数不能很好地拟合观测数据的真实多维度,不应进行定量解释。我们在盐渍化背景下的实际AEM调查中展示了我们的方法,揭示了淡水-盐水界面中的问题区域。有趣的是,有问题的区域不一定在更大的深度,而是在界面发生变化的地方。我们的方法的优点是所有的计算都可以在一台笔记本电脑上实现。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessing Quantitatively Interpretable Zones From 1D Forward Modelling Aem Inversion Models
The inversion of time-domain AEM data with full 3D inversion requires specialists’ expertise and a huge amount of computational resources, not readily available to everyone. Consequently, quasi-2D/3D inversion methods are prevailing, using a much faster but approximate (1D) forward model. The question remains whether the obtained inversion results are reliable and can be interpreted quantitatively. We propose an appraisal tool for quasi-2D/3D methods that indicate zones in the inversion model that are not in agreement with the multidimensional (2D/3D) forward model and therefore, should not be interpreted in a quantitative fashion. The image appraisal step only requires one full 2.5D or 3D forward and one multidimensional Jacobian computation on a coarse mesh to compute a so-called normalized gradient. Large values in that gradient indicate model parameters that do not fit the true multidimensionality of the observed data well and should not be interpreted quantitatively. We demonstrate our method on a real AEM survey in a salinization context, revealing problematic zones in the fresh-saltwater interface. Interestingly, the problematic zones are not necessarily at larger depths, but where the interface is changing. The advantage of our approach is that all computations are feasible on a single laptop.
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