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The use of reference models from a priori data to guide 2D inversion of electrical resistivity tomography data

机译:使用先验数据中的参考模型来指导电阻层析成像数据的二维反演

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Clay-rich till plains cover much of the UK. Such sites are attractive locations for landfills, since clay aquitards lower the risk of landfill leachate entering groundwater. However, such tills often contain sand and gravel bodies that can act as leachate flow routes. Such bodies may not be detected by conventional site investigation techniques such as drilling boreholes and trial pitting. A method of guided inversion, where a priori data are used to construct structural reference models for use in inverting electrical resistivity tomography data, was proposed as a tool to improve the detection of sand and gravel bodies within clay-rich till sequences.rnFollowing a successful 2D guided inversion synthetic modelling study, a field study was undertaken. Wenner 2D electrical resistivity tomography lines, resistivity cone penetrometry bores and electromagnetic induction ground resistivity data were collected over a site on the East Yorkshire coast, England, where sand and gravel lenses were known to exist from cliff exposures. A number of equally valid geoelectrical models were constructed using the electromagnetic and resistivity cone data. These were used as structural reference models in the inversion of the resistivity tomography data. Blind inversion using an homogenous reference model was also carried out for comparison.rnIt was shown for the first time that the best solution model produced by 2D inversion of one data set with a range of structural reference models could be determined by using the l_2 model misfit between the solution models and associated reference models (reference misfit) as a proxy for the l_2 misfit between the solution models and the synthetic model or 'best-guess' geoelectrical model (true misfit). The 2D methodology developed here is applicable in clay-rich till plains containing sand and gravel bodies throughout the UK.
机译:粘土丰富的平原覆盖了英国大部分地区。这些地点是垃圾填埋场的诱人地点,因为粘土无水果汁降低了垃圾填埋场渗滤液进入地下水的风险。但是,这样的耕till通常包含可以用作渗滤液流动路线的沙子和砾石体。通过常规的现场调查技术(如钻孔和试点)可能无法检测到此类物体。有人提出了一种引导反演的方法,该方法使用先验数据来构建用于将电阻率层析成像数据反演的结构参考模型,以此作为一种工具来改进对富含粘土的土层中砂石砾石体的检测.rn进行了二维导向反演综合建模研究,进行了实地研究。在英格兰东约克郡海岸的一个地点收集了Wenner 2D电阻率层析成像线,电阻率锥孔法测孔和电磁感应地面电阻率数据,该处已知因悬崖暴露而存在沙石砾石。利用电磁和电阻率锥数据构造了许多同样有效的地电模型。这些被用作电阻率层析成像数据反演中的结构参考模型。还进行了使用同质参考模型的盲反演以进行比较。rn首次表明,可以通过使用l_2模型失配来确定一个数据集与一系列结构参考模型的二维反演所产生的最佳解决方案模型解决方案模型和关联的参考模型之间的差异(参考错配),作为解决方案模型与合成模型或“最佳猜测”地电模型(真实错配)之间的l_2错配的代理。此处开发的2D方法适用于整个英国富含粘土的平地,其中包含沙子和砾石体。

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  • 来源
    《Geophysical Prospecting》 |2009年第6期|1035-1048|共14页
  • 作者单位

    Reynolds Geo-Sciences Ltd, Wales, CH7 1XP, UK;

    Scbool of Earth and Environment, University of Leeds, Woodbouse Lane, Leeds LS2 9JT, UK;

    Scbool of Earth and Environment, University of Leeds, Woodbouse Lane, Leeds LS2 9JT, UK;

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