Spatial organization of biomass controls intrinsic permeability of porous systems
Wenqiao Jiao, David Scheidweiler, Nolwenn Delouche, Alberto Guadagnini, Pietro de Anna
TL;DR
The study shows that biomass growth in porous media reduces permeability, but the spatial arrangement of biomass—driven by bacterial motility—controls the extent of hydraulic decline more than total biomass. Using a microfluidic porous chip under a fixed pressure gradient and time-lapse fluorescence, the authors compare motile and non-motile Pseudomonas putida and link pore-scale biomass distributions to macroscopic permeability $k_t(t)$ through a mechanistic two-pathway model. The model, characterized by a single fitting parameter $k_{bf}$, accurately predicts permeability dynamics from pore-scale data, demonstrating $k_t(t)$ can be derived from biomass distribution patterns and that $k_{bf} \approx 2.5$ Darcy best fits both strains. These findings reveal that biomass spatial organization—shaped by motility—determines clogging efficiency and have practical implications for filtration, water treatment, soil bioremediation, and oil recovery where controlling flow through biomass is essential.
Abstract
Biofilms in porous media critically influence hydraulic properties in environmental and engineered systems. However, a mechanistic understanding of how microbial life controls permeability remains elusive. By combining microfluidics, controlled pressure gradient and time-lapse microscopy, we quantify how motile and non-motile bacteria colonize a porous landscape and alter its resistance to flow. We find that while both strains achieve nearly identical total biomass, they cause drastically different permeability reductions - 78% for motile cells versus 94% for non-motile cells. This divergence stems from motility, which limits biomass spatial accumulation, whereas non-motile cells clog the entire system. We develop a mechanistic model that accurately predicts permeability dynamics from the pore-scale biomass distribution. We conclude that the spatial organization of biomass, not its total amount, is the primary factor controlling permeability.
