Data-driven hydrogeophysical and redox modelling

N. Claes, N. Foged, T. Vilhelmsen, R. R. Frederiksen, H. Kim, A. Christiansen
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Abstract

Summary Detailed 3D structural information of the subsurface is fundamental for development of both the hydrological and the geochemical models that can be used for analysis of nitrate reduction processes in the subsurface and targeted nitrate regulation. In some areas data, coverage might be sparse or suffering from bad data quality, which results in information gaps. We suggest therefore a workflow that merges tTEM resistivity data and borehole lithologies, and uses these datasets to generate an ensemble of equally plausible 3D models of hydrogeological units and redox conditions. In an initial step the input datasets are merged via accumulated clay thickness modeling. This dataset is in a second step transformed into a training image, that is to be used in multipoint statistical simulations. The application of Direct Sampling within this workflow allows for simultaneous simulation of these variables. This approach allows for retaining the complex geostatistical spatial relationships that can exist between the different datasets in the resulting generated 3D models.
数据驱动的水文地球物理和氧化还原模拟
详细的地下三维结构信息是开发水文和地球化学模型的基础,可用于分析地下硝酸盐还原过程和有针对性的硝酸盐调节。在某些领域,数据覆盖范围可能很稀疏或数据质量差,从而导致信息缺口。因此,我们建议采用一种将瞬变电磁法电阻率数据与井眼岩性相结合的工作流程,并使用这些数据集生成一套同样可信的水文地质单元和氧化还原条件的3D模型。在初始阶段,通过累积粘土厚度建模合并输入数据集。第二步,将该数据集转换为训练图像,用于多点统计模拟。直接采样在此工作流程中的应用允许同时模拟这些变量。这种方法允许在生成的3D模型中保留不同数据集之间存在的复杂地质统计空间关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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