基于瞬变电磁法测量和静态位移校正的VES模型改进。:埃及的案例研究

M. M. Osman, G. El-Qady, Th. Abdel Fattah, M. Rashed, M. Mohamdeen
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引用次数: 1

摘要

近地表电导率的变化,例如小的局部三维(3D)体的存在,会导致直流(DC)中的电畸变,因此测量的视电阻率受到对数尺度上称为静态位移的恒定位移的影响。在这项研究中,我们使用电磁测深技术来校正仅影响电阻率数据的静态位移。之所以使用“静态位移”一词,是因为视电阻率在对数尺度上被一个恒定的位移值(S)所扭曲,这导致了误导性的解释。注意到两组数据在同一位置的测深曲线具有一致的模式。注意到在排除地震勘探数据移位之前,地震勘探和瞬变电磁法一维反演模型不匹配的问题。将瞬变电磁法和瞬变电磁法测量结果表示在同一张图上,然后计算瞬变电磁法曲线的位移因子S,使其与瞬变电磁法曲线直接重叠。去掉平移因子后的ve曲线一维反演模型与TEM一维模型数据吻合。
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Enhancement the VES models based on the TEM measurements and the application of static shift corrections.: case study from Egypt
ABSTRACT Variations in conductivity in the near-surface, such as the presence of small and localized three-dimensional (3D) bodies, cause a galvanic distortion in direct current (DC), so the measured apparent resistivity is affected by a constant shift on a log scale called Static Shift. In this study, We used electromagnetic sounding techniques to correct for the static shift affecting the electric resistivity data only. The term “static shift” is used because apparent resistivity is distorted by a constant, shifting value (S) on a log scale, which lead to misleading interpretation. It was noticed that the two data sets' sounding curves at the same location have a concordant pattern. The problem was noticed in the 1D inversion models for VES and TEM were not matched together before removal of VES data shift. The TEM and VES measurements are represented on the same graph, then the shifting factor (S) is calculated for the VES curves to directly overlap the TEM curve. The 1D inversion model for VES curves after removing the shifting factor shows matched data with the TEM 1D model.
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