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Hydrogeological Model Selection Among Complex Spatial Priors

机译:复杂空间先验中的水文地质模型选择

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摘要

Hydrogeological field studies rely often on a single conceptual representation of the subsurface. This is problematic since the impact of a poorly chosen conceptual model on predictions might be significantly larger than the one caused by parameter uncertainty. Furthermore, conceptual models often need to incorporate geological concepts and patterns in order to provide meaningful uncertainty quantification and predictions. Consequently, several geologically realistic conceptual models should ideally be considered and evaluated in terms of their relative merits. Here, we propose a full Bayesian methodology based on Markov chain Monte Carlo to enable model selection among 2-D conceptual models that are sampled using training images and concepts from multiple-point statistics. More precisely, power posteriors for the different conceptual subsurface models are sampled using sequential geostatistical resampling and Graph Cuts. To demonstrate the methodology, we compare and rank five alternative conceptual geological models that have been proposed in the literature to describe aquifer heterogeneity at the MAcroDispersion Experiment site in Mississippi, USA. We consider a small-scale tracer test for which the spatial distribution of hydraulic conductivity impacts multilevel solute concentration data observed along a 2-D transect. The thermodynamic integration and the stepping-stone sampling methods were used to compute the evidence and associated Bayes factors using the computed power posteriors. We find that both methods are compatible with multiple-point statistics-based inversions and provide a consistent ranking of the competing conceptual models considered.
机译:水文地质现场研究通常依赖于地下的单一概念表示。这是有问题的,因为选择不佳的概念模型对预测的影响可能远大于参数不确定性所造成的影响。此外,概念模型通常需要结合地质概念和模式,以便提供有意义的不确定性量化和预测。因此,理想情况下应考虑和评估几个地质上现实的概念模型,并考虑其相对优点。在这里,我们提出了一个基于马尔可夫链蒙特卡洛的完整贝叶斯方法,以使能够从训练图像和多点统计中提取的2D概念模型中进行模型选择。更准确地说,使用顺序地统计重采样和图割对不同概念地下模型的后验功率进行采样。为了证明该方法,我们比较并排名了文献中提出的五个替代性概念地质模型,这些模型描述了美国密西西比州MAcroDispersion实验现场的含水层非均质性。我们考虑一个小规模的示踪剂测试,其水力传导率的空间分布会影响沿二维断面观察到的多级溶质浓度数据。使用热力学积分和垫脚石采样方法,使用计算出的功率后验来计算证据和相关的贝叶斯因子。我们发现这两种方法都与基于多点统计的反演兼容,并且为所考虑的竞争概念模型提供了一致的排名。

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  • 来源
    《Water resources research》 |2019年第8期|6729-6753|共25页
  • 作者单位

    Univ Lausanne Inst Earth Sci Appl & Environm Geophys Grp Lausanne Switzerland;

    British Geol Survey Environm Sci Ctr Nottingham England;

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  • 正文语种 eng
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