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Geo-electrical data fusion by stochastic co-conditioning simulations for delineating groundwater protection zones

机译:基于随机协同条件模拟的地电数据融合,勾勒出地下水保护区

摘要

In hydrogeology, advances in the delimitation of protection zones are made by the use of stochastic simulations integrating all available data. In practice, due to the few available measurements of the main parameters (hard data), it is very useful to integrate several secondary properties of the media as indirect data (soft data) to reduce the uncertainty of the results. In aquifers, most of the solute spreading is governed by the hydraulic conductivity (K) spatial variability, which is generally considered as the main uncertain parameter. A stochastic approach integrating hydraulic conductivity measurements (hard data), head observations and shallow electrical resistivity tomography (soft data) is presented. Results are discussed on a synthetic and on a practical case. It is shown in practice how the uncertainty of the well capture zone probability distribution (CaPD) can be reduced. Since geophysical data and head observations are easier to collect on the field then hydraulic conductivity measurements, they are generally more abundant. The methodology presented can even be used in real applications when little or no information is available about the hydraulic properties, through the conditioning on geophysical data and/or head observations.
机译:在水文地质学中,通过使用整合所有可用数据的随机模拟,在保护区划界方面取得了进展。在实践中,由于主要参数(硬数据)的可用测量很少,因此将介质的几个次要特性作为间接数据(软数据)进行集成以减少结果的不确定性非常有用。在含水层中,大多数溶质扩散是由水力传导率(K)空间变异性决定的,该系数通常被认为是主要的不确定参数。提出了一种将水力传导率测量(硬数据),水头观测和浅层电阻率层析成像(软数据)集成在一起的随机方法。在综合和实际案例中讨论了结果。在实践中表明,如何减少井捕获区概率分布(CaPD)的不确定性。由于地球物理数据和头部观测资料比水力传导率测量资料更容易在现场收集,因此它们通常更为丰富。通过对地球物理数据和/或头部观测资料进行条件处理,即使很少或没有关于水力特性的信息,所提出的方法甚至可以用于实际应用中。

著录项

  • 作者

    Dassargues, Alain;

  • 作者单位
  • 年度 2006
  • 总页数
  • 原文格式 PDF
  • 正文语种 en
  • 中图分类

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