Pore‐Scale Segregation and Enrichment of Polydisperse Colloids via Transverse Migration in Porous Media

Abstract Understanding transport of anomalous colloids and contaminants requires partition of polydisperse colloids at the pore scale. Using a high‐resolution dual‐mode microscopy system, we directly visualize cross‐sectional concentration profiles. Furthermore, we identify a previously overlooked phenomenon: the occurrence of persistent transverse concentration heterogeneity and centerline enrichment above the injected concentration ( C/C 0 > 1) during transport. Observations at different spatial and temporal scales reveal transverse colloid migration during anomalous segregation and enrichment of colloids. These observations revealed that colloid transport results in the formation of distinct concentration‐defined regions that cannot be inferred from conventional solute transport behavior. We establish a double‐erf logarithmic‐gradient criterion to delineate the main‐flow and diffusion zones and quantify the main‐flow ratio (). This criterion defines transport zones directly from the observed concentration gradients, avoiding the nonuniqueness of conventional inversion‐based two‐zone models. Our results provide direct pore‐scale evidence and a quantitative framework linking pore‐scale transport structure to macroscopic behavior.

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Publication Details

Journal
Geophysical Research Letters
Published
2026-11-06
DOI
https://doi.org/10.1029/2026gl126367
Primary Topic
Groundwater flow and contamination studies
Type
article
Field-Weighted Citation Impact
0.00

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article

Pore‐Scale Segregation and Enrichment of Polydisperse Colloids via Transverse Migration in Porous Media

Qiwen Xia, Zhen Chen, Jinpei Hu, Jiangtao He et al.
Geophysical Research Letters
Groundwater flow and contamination studies
article

Pore‐Scale Segregation and Enrichment of Polydisperse Colloids via Transverse Migration in Porous Media

Qiwen Xia, Zhen Chen, Jinpei Hu, Jiangtao He, Baonan He, Yanjia Chu, Zhenjun Zhou, Zirong Liu, Xiaojun Li
article en

Abstract

Abstract Understanding transport of anomalous colloids and contaminants requires partition of polydisperse colloids at the pore scale. Using a high‐resolution dual‐mode microscopy system, we directly visualize cross‐sectional concentration profiles. Furthermore, we identify a previously overlooked phenomenon: the occurrence of persistent transverse concentration heterogeneity and centerline enrichment above the injected concentration ( C/C 0 > 1) during transport. Observations at different spatial and temporal scales reveal transverse colloid migration during anomalous segregation and enrichment of colloids. These observations revealed that colloid transport results in the formation of distinct concentration‐defined regions that cannot be inferred from conventional solute transport behavior. We establish a double‐erf logarithmic‐gradient criterion to delineate the main‐flow and diffusion zones and quantify the main‐flow ratio (). This criterion defines transport zones directly from the observed concentration gradients, avoiding the nonuniqueness of conventional inversion‐based two‐zone models. Our results provide direct pore‐scale evidence and a quantitative framework linking pore‐scale transport structure to macroscopic behavior.

Geophysical Research LettersVol. 53(21)
China University of Geosciences (Beijing) (CN)
National Natural Science Foundation of China
Openalex Percentile: Top 25%
Groundwater flow and contamination studies
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