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Geological realism in hydrogeological and geophysical inverse modeling: a review

机译:水文地质和地球物理反演模拟中的地质现实主义:   回顾

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摘要

Scientific curiosity, exploration of georesources and environmental concernsare pushing the geoscientific research community toward subsurfaceinvestigations of ever-increasing complexity. This review explores variousapproaches to formulate and solve inverse problems in ways that effectivelyintegrate geological concepts with geophysical and hydrogeological data. Moderngeostatistical simulation algorithms can produce multiple subsurfacerealizations that are in agreement with conceptual geological models andstatistical rock physics can be used to map these realizations into physicalproperties that are sensed by the geophysical or hydrogeological data. Theinverse problem consists of finding one or an ensemble of such subsurfacerealizations that are in agreement with the data. The most general inversionframeworks are presently often computationally intractable when applied tolarge-scale problems and it is necessary to better understand the implicationsof simplifying (1) the conceptual geological model (e.g., using modelcompression); (2) the physical forward problem (e.g., using proxy models); and(3) the algorithm used to solve the inverse problem (e.g., Markov chain MonteCarlo or local optimization methods) to reach practical and robust solutionsgiven today's computer resources and knowledge. We also highlight the need tonot only use geophysical and hydrogeological data for parameter estimationpurposes, but also to use them to falsify or corroborate alternative geologicalscenarios.
机译:科学的好奇心,对地质资源的探索以及对环境的关注正推动着地球科学研究界朝着越来越复杂的地下研究方向发展。这篇综述探索了各种方法来制定和解决反问题,从而有效地将地质概念与地球物理和水文地质数据相结合。现代地统计学模拟算法可以产生与概念地质模型相符的多个地下实现,并且统计岩石物理学可用于将这些实现映射到由地球物理或水文地质数据感测到的物理特性。反问题包括找到与数据一致的一种或多种这样的地下实现。当前,最普遍的反演框架在应用于大规模问题时通常在计算上难以处理,因此有必要更好地理解简化(1)概念性地质模型(例如,使用模型压缩)的含义; (2)物理转发问题(例如,使用代理模型); (3)用于解决反问题的算法(例如,马尔可夫链蒙特卡洛法或局部优化方法),以根据当今的计算机资源和知识获得实用且可靠的解决方案。我们还强调了不仅需要将地球物理和水文地质数据用于参数估计目的,而且需要使用它们来伪造或证实其他地质情况。

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