19–22 May 2026
Europe/Paris timezone

Dynamic Bioclogging in Heterogeneous Porous Media: The Role of Biofilm Micro-Permeability and Shear-Driven Detachment

22 May 2026, 10:20
1h 30m
Poster Presentation (MS20) Special Session in Honor of Jun Yao Poster

Speaker

Chuang Ning

Description

Bioclogging alters permeability through the coupled evolution of pore-scale hydrodynamics, pore structure, and biofilm morphology during biofilm growth. Many pore-scale models treat biofilms as impermeable solids and neglect shear-driven detachment under spatially non-uniform flow, which can bias predictions of residual permeability in heterogeneous porous media. Here we develop an improved coupled LBM–IBM–CA (lattice Boltzmann–immersed boundary–cellular automata) model that represents biofilms as a microporous phase with finite permeability and updates growth and detachment dynamically as clogging progresses. Heterogeneous pore structures are generated using Gaussian statistics, and biofilm micro-permeability is incorporated via a Brinkman-type drag formulation to permit intra-biofilm flow and associated pressure redistribution. We conduct parametric simulations spanning pore-structure heterogeneity and biofilm permeability to quantify their nonlinear coupling with shear detachment. Biofilm growth is advanced by cellular-automata rules, while detachment is triggered when local interfacial shear exceeds a prescribed criterion, allowing the feedback between preferential flow and erosion to emerge naturally. Simulations show that structural heterogeneity promotes preferential flow paths and produces intermittent high-shear regions at biofilm–fluid interfaces; in the impermeable-biofilm formulation, these shear peaks lead to frequent detachment events and pronounced oscillations in permeability. When biofilm permeability is included, intra-biofilm flow reduces near-interface velocity gradients and interfacial shear, providing a hydraulic buffering mechanism that stabilizes biofilm retention in high-shear zones. Consequently, permeability trajectories exhibit substantially damped fluctuations and converge to a more stable residual hydraulic conductivity, even with higher retained biomass. These results underscore the importance of representing biofilm micro-permeability and shear detachment for pore-scale prediction of bioclogging dynamics in strongly heterogeneous porous media.

Country China
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Authors

Chuang Ning Junjie Zhong (China university of petroleum (east China))

Co-authors

Shanchao Liu (China university of petroleum (east China)) lilong Xu (China university of petroleum (East China)) Mr Junhao Wu (China University of Petroleum (East China)) Mr Junhui Liu (China University of Petroleum (East China)) Jun Yao (China University of Petroleum) Prof. Hai Sun (China University of Petroleum (East China)) Prof. Yongfei Yang (China University of Petroleum (East China)) Lei Zhang (China University of Petroleum (East China))

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