4.7 Article

Anomalous transport of colloids in heterogeneous porous media: A multi-scale statistical theory

期刊

JOURNAL OF COLLOID AND INTERFACE SCIENCE
卷 617, 期 -, 页码 94-105

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.jcis.2022.02.127

关键词

Colloid; Porous media; Multi-scale approach; Anomalous transport; Digital rock

资金

  1. Science4CleanEnergy European research consortium - European Unions Horizon 2020 research and innovation programme [764810]
  2. UCL Chemical Engineering Department

向作者/读者索取更多资源

In this study, the transport behavior of suspended colloids in heterogeneous porous media is investigated through core-flooding experiments and computational simulations. It is found that the observed anomalous transport is particle-type dependent and arises from the microscopic dispersion and deposition of particles in heterogeneous flow fields. The study also presents a residence-time distribution function that captures the entire transition from pre-asymptotic to asymptotic behavior, providing valuable insights for interpreting experimental data and designing colloidal tracers.
Hypothesis: Transport of suspended colloids in heterogeneous porous media is a multi-scale process that exhibits anomalous behavior and cannot be described by the Fickian dispersion theory. Although many studies have documented colloids' transport at different length scales, a theoretical basis that links pore-to core-scale observations remains lacking. It is hypothesized that a recently proposed pore scale statistical kinetic theory is able to capture the results observed experimentally.Experiments: We implement a multi-scale approach via conducting core-flooding experiments of colloidal particles in a sandstone sample, simulating particles flowing through a sub-volume of the rock's digital twin, and developing a core-scale statistical theory for particles' residence times via upscaling the pore-scale kinetic theory. Experimental and computational results for solute transport are used as benchmark.Findings: Based on good agreement across the scales achieved in our investigation, we show that the macroscopically observed anomalous transport is particle-type dependent and stems from particles' microscopic dispersion and deposition in heterogeneous flow fields. In particular, we reveal that residence-time distributions (i.e., breakthrough curve) obey a closed-form function that encompasses particles' microscopic dynamics, which allows investigations of a whole transition from pre asymptotic to asymptotic behavior. The physical insights attained could be useful for interpreting experimental data and designing colloidal tracers.(c) 2022 Elsevier Inc. All rights reserved.

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