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Geoelectrical inference of mass transfer parameters using temporal moments

机译:利用时间矩对传质参数进行地电推断

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摘要

We present an approach to infer mass transfer parameters based on (1) an analytical model that relates the temporal moments of mobile and bulk concentration and (2) a bicontinuum modificaijon to Archie's law. Whereas conventional geochemical measurements preferentially sample from the mobile domain, electrical-resistivity tomography (ERT) is sensitive to bulk electrical conductivity and, thus, electrolytic solute in both the mobile and immobile domains. We demonstrate the new approach, in which temporal moments of collocated mobile domain conductivity (i.e., conventional sampling) and ERT-estimated bulk conductivity are used to calculate heterogeneous mass transfer rate and immobile porosity fractions in a series of numerical column experiments.
机译:我们提出了一种基于(1)与流动和体积浓度的瞬时矩相关的分析模型,以及(2)与阿奇定律有关的双连续谱修正来推断传质参数的方法。常规的地球化学测量优先从移动区域采样,而电阻层析成像(ERT)对整体电导率敏感,因此对移动和固定区域中的电解溶质都敏感。我们展示了一种新方法,其中在一系列数值柱实验中,并置的移动域电导率(即常规采样)和ERT估计的体积电导率的瞬时矩用于计算非均质传质速率和固定孔隙率分数。

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