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Inversion of concentric loop electromagnetic data by transformation to an equivalent potential field response

机译:通过转换为等效电位场响应来反转同心环电磁数据

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A novel approach to the inversion of concentric loop electromagnetic (EM) data is through transformation of moving-source EM data to an equivalent fixed-source potential field. This equivalent potential field has been named as the surrogate potential field. The proposed approach then provides for example, efficient target depth estimates through Euler deconvolution. Under the quasi-static approximation, at each instant in the earth, diffuse loops of induced current are the source of the recorded response. Successive samples of the magnetic field of confined current loops can be mathematically manipulated to create a surrogate potential field from an equivalent constant induced current, as the surrogate potential field is proportional to the square root of the concentric loop EM response. Processing includes inspecting data and correcting for the sign ambiguity at suitably stable locations. Correct surrogate potential field transformation relies on induced current systems being geometrically fixed in location, and as such will be predominantly correct for tabular conductors that are of relatively small size. For these small targets, stitched ID layered-earth EM inversions often overestimate the depth of a small near-surface body. Unconfined currents induced in conductive overburden introduce a 'background' which requires subtraction before transformation to a surrogate potential. Confidence limits on solutions are part of a least-squares regression involving a cluster analysis. These form the basis for evaluation of the reliability with which the proposed method has estimated the target parameters from EM data. Successful estimations of target depth and location have been performed for synthetic horizontal and vertical tabular plate models, and with limitations for compact bodies represented by a spherical conductor. Three case studies illustrate the characteristics of the proposed method, illustrating useful results with limitations arising in field data and its processing.
机译:同心环电磁(EM)数据反演的一种新颖方法是将移动源EM数据转换为等效的固定源电势场。该等效势场已被称为替代势场。然后,所提出的方法例如通过欧拉反卷积提供有效的目标深度估计。在准静态近似下,在地球上的每个时刻,感应电流的扩散回路都是记录的响应的来源。由于替代电位场与同心环EM响应的平方根成正比,因此可以数学方式对连续电流回路的磁场的连续样本进行操作,以根据等效的恒定感应电流创建替代电位场。处理过程包括检查数据并在适当的稳定位置纠正符号歧义。正确的替代势场转换依赖于在几何上位置固定的感应电流系统,因此,对于尺寸相对较小的板状导体,这将是主要正确的方法。对于这些小型目标,缝合的ID层状地球EM反演通常会高估小型近地物体的深度。导电覆盖层中感应的无限制电流会引入“背景”,在转换为替代电位之前需要先减去。解决方案的置信限是涉及聚类分析的最小二乘回归的一部分。这些构成了评估可靠性的基础,所提出的方法可用来从EM数据估计目标参数。对于合成的水平和垂直板状板模型,已经成功地估计了目标深度和位置,并且对以球形导体为代表的紧凑型实体存在局限性。三个案例研究说明了所提出方法的特征,说明了有用的结果,但在现场数据及其处理方面存在局限性。

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