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首页> 外文期刊>Journal of Applied Geophysics >Estimation of the electrical potential distribution along metallic casing from surface self-potential profile
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Estimation of the electrical potential distribution along metallic casing from surface self-potential profile

机译:从表面自电势分布估算沿金属套管的电势分布

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Corroding casings of wells generate negative self-potential (SP) anomalies, increasing from about 10 to -500 mV in the vicinity of the well to 0 mV at large distances. As reported in previous laboratory experiment, SP can be used to retrieve the distribution of electrical potential along the casing, which is somehow a proxy for the corrosion state of the casing. These studies used 3D (whole space) or surface 2D (whole surface) measurements of SP distribution; here we reported a field example, for which only a 1D surface SP profile is available. In order to retrieve the most probable associated potential distribution (defined by a spline) along the 11.1-m long metallic casing, we develop a direct model based on geometrical and geoelectrical properties of the medium, which was then used in a (non-deterministic) optimization procedure by simulated annealing, including some physical constrains. Tests carried out on a synthetic case allowed the initial source to be correctly retrieved, provided that the number of nodes used for the spline defining the potential distribution along the casing is large enough. The inversion of real field data provided a dipolar anomaly, with minimal negative amplitude of around -600 mV at 5 m, and maximal positive amplitude of about 1100 mV at 9 m (close to the level of the water table), this shape being in agreement with the results of previous laboratory studies. (C) 2016 Elsevier B.V. All rights reserved.
机译:井的腐蚀套管产生负自电势(SP)异常,从井附近的约10到-500 mV增加到大距离处的0 mV。如先前实验室实验中报道的那样,SP可用于检索沿套管的电势分布,这在某种程度上可以替代套管的腐蚀状态。这些研究使用了SP分布的3D(整个空间)或表面2D(整个表面)测量。在这里,我们报告了一个现场示例,该示例仅提供一维表面SP轮廓。为了检索沿11.1 m长的金属套管的最可能的关联电势分布(由样条线定义),我们基于介质的几何和地电特性开发了直接模型,然后将其用于(不确定性) )通过模拟退火(包括一些物理约束)来优化程序。如果在样条上定义沿套管的电位分布的节点数足够大,则可以对合成案例进行测试,以正确检索初始源。实地数据的反演提供了一个偶极异常,在5 m处的最小负振幅约为-600 mV,在9 m处的最大正振幅约为1100 mV(接近地下水位),这种形状处于与以前的实验室研究结果一致。 (C)2016 Elsevier B.V.保留所有权利。

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