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SQUARE ARRAY RESISTIVITY ANOMALIES AND INHOMOGENEITY RATIO CALCULATED BY THE FINITE-ELEMENT METHOD

机译:有限元法计算的方形阵列电阻率异常和非均质比

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摘要

In this work the square array configuration is studied. As with any four-electrode measuring configuration, three different resistances can be measured directly and, in particular, by using the square array these resistance values can be used to obtain a measure of the apparent anisotropy: this is the so-called azimuthal inhomogeneity ratio (AIR). The AIR is used widely to derive information regarding the directional variation of the subsurface resistivity. Similar types of information can be obtained using any collinear array but would need to be used in a crossed mode. This gives an operational advantage to the square array. Here, the AIR and the square alpha and beta apparent resistivities have been calculated for a number of simple subsurface models. Moreover, the apparent resistivity responses for several different linear arrays were calculated to allow useful comparisons. The forward modeling has been carried out via a 2.5-D finite-element scheme and an existing approach has been modified in order to calculate the potential variations parallel to the strike direction. Here, the use of AIR as a pattern recognition tool is investigated. The AIR anomalies are shown to delineate the edges of the targets successfully, retaining the same pattern when the model was shifted in depth, and indicating a satisfactory resolving ability. The AIR can be used as complementary information to the apparent resistivity measures and can improve the interpretation. However, careful consideration has to be given to the data noise. [References: 18]
机译:在这项工作中,对方形阵列的配置进行了研究。与任何四电极测量配置一样,可以直接测量三个不同的电阻,特别是通过使用正方形阵列,这些电阻值可以用来获得表观各向异性的量度:这就是所谓的方位不均匀率(空气)。 AIR被广泛用于导出有关地下电阻率方向变化的信息。可以使用任何共线数组获得类似类型的信息,但需要以交叉模式使用。这为方形阵列提供了操作优势。在这里,已经为许多简单的地下模型计算了AIR以及平方的α和β视在电阻率。此外,计算了几种不同线性阵列的视在电阻率响应,以便进行有用的比较。通过2.5D有限元方案进行了正向建模,并对现有方法进行了修改,以便计算平行于打击方向的电位变化。在这里,研究了使用AIR作为模式识别工具。 AIR异常显示成功地描绘了目标的边缘,当模型在深度上移动时保持了相同的模式,并表明令人满意的解析能力。 AIR可以用作视电阻率测量的补充信息,并可以改善解释。但是,必须仔细考虑数据噪声。 [参考:18]

著录项

  • 来源
    《Geophysics》 |1997年第2期|p. 426-435|共10页
  • 作者单位

    ARISTOTELIAN UNIV THESSALONIKI GEOPHYS LAB GR-54006 THESSALONIKI GREECE;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

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