反演(地质)
地下水
比例(比率)
地质学
地下水模型
环境科学
地球物理学
含水层
地貌学
地下水补给
地图学
岩土工程
地理
构造盆地
作者
Amanda Triplett,Andrew Bennett,Laura E. Condon,P. Melchior,R. M. Maxwell
摘要
Abstract Hydrogeologic models generally require gridded subsurface properties, however these inputs are often difficult to obtain and highly uncertain. Parametrizing computationally expensive models where extensive calibration is computationally infeasible is a long standing challenge in hydrogeology. Here we present a machine learning framework to address this challenge. We train an inversion model to learn the relationship between water table depth and hydraulic conductivity using a small number of physical simulations. For a 31M grid cell model of the US we demonstrate that the inversion model can produce a reliable K field using only 30 simulations for training. Furthermore, we show that the inversion model captures physically realistic relationships between variables, even for relationships that were not directly trained on. While there are still limitations for out of sample parameters, the general framework presented here provides a promising approach for parametrizing expensive models.
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