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Characterization of Aquifer Hydraulic Parameters: from Theis to Hydraulic Tomography

机译:含水层水力参数的表征:从泰斯到水力层析成像

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摘要

Groundwater is in many parts of the world an important source of fresh water for several purpose such as domestic and industrial use and irrigation. Pollution and bad management of groundwater are only two of the problems that affect the aquifers around the world. Detailed information about the spatial distribution of hydraulic properties in subsurface are of crucial importance for a proper management of groundwater and for the prediction of the solutes transport in aquifer and therefore for the design of effective remediation systems. Different methods have been used for characterizing aquifer hydraulic parameters but the most used are the interpretation of the pumping tests. They consist of measuring the drawdowns in an observation well due to the extraction of a constant rate of water from a different well. The data collected in this way are then fitted with analytical solutions that assume aquifer homogeneity so providing average values of the hydraulic parameters without considering any spatial distribution. In the last 15 years, to remove the homogeneity hypothesis and to investigate the spatial distribution of aquifer hydraulic properties, a technique called Hydraulic Tomography has been developed. It consists of sequential aquifer tests in which the stress location is sequentially moved and the hydraulic responses are monitored in other locations. The data collected are then used to solve an inverse problem and to obtain information about the spatial variability of the aquifer hydraulic parameters. In this work after a discussion of the traditional aquifer tests and an overview of the inverse methods applied to the hydraulic tomography, a Bayesian Geostatistical approach (conditioned on direct head data) is considered and tested with tomographic data in transient flow conditions and with both constant and non-stationary boundary conditions. Traditional analyses and the hydraulic tomography approach are then applied to a real case of the well field of the AIPO Boretto Research Site (Northern Italy) to test the methodologies on a field application. To date, the application of the Bayesian Geostatistical approach to inverse problems (in particular on real problems) is limited by the lack of tools available for the scientific and technical community. For this reason the USGS (United States Geological Survey) is sponsoring a project to incorporate the Bayesian approach as a module of the industry standard software package PEST for the parameters estimation. In this work the kernel of the Bayesian PEST developed by the Writer is described. This module is doubtless a good way to spread the Bayesian Geostatistical inverse procedure to the modelers community.
机译:在世界许多地区,地下水是用于家庭和工业用途以及灌溉等多种目的的重要淡水来源。地下水的污染和管理不善只是影响全世界含水层的两个问题。有关地下水力特性空间分布的详细信息对于正确管理地下水,预测含水层中的溶质运移以及因此设计有效的修复系统至关重要。已经使用了不同的方法来表征含水层的水力参数,但是最常用的方法是对抽水试验的解释。它们包括测量观测井中的水位下降,这是因为从另一口井中提取了恒定的水量。然后,以这种方式收集的数据将采用假设含水层均匀性的分析解决方案,从而在不考虑任何空间分布的情况下提供水力参数的平均值。在过去的15年中,为消除均一性假设并研究含水层水力特性的空间分布,开发了一种称为“液压层析成像”的技术。它由顺序含水层测试组成,其中应力位置顺序移动,并且在其他位置监测水力响应。然后将收集的数据用于解决反问题,并获得有关含水层水力参数空间变异性的信息。在讨论了传统的含水层测试和对液压层析成像的反演方法进行了概述之后的这项工作中,考虑了贝叶斯地统计方法(以直接水头数据为条件),并在瞬变流动条件下以及在两者均恒定的情况下,对层析成像数据进行了测试。和非平稳边界条件。然后,将传统分析和液压层析成像方法应用于AIPO Boretto研究站点(意大利北部)井场的真实案例,以测试现场应用的方法学。迄今为止,由于缺乏科学和技术界可用的工具,贝叶斯地统计学方法在反问题(特别是在实际问题上)的应用受到限制。因此,USGS(美国地质调查局)赞助了一个项目,该项目将贝叶斯方法纳入了用于参数估计的行业标准软件包PEST的模块中。在这项工作中,描述了作者编写的贝叶斯PEST内核。无疑,该模块是将贝叶斯地统计逆过程推广到建模者社区的好方法。

著录项

  • 作者

    DOria Marco;

  • 作者单位
  • 年度 2010
  • 总页数
  • 原文格式 PDF
  • 正文语种 Inglese
  • 中图分类

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