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Enhanced manganese oxidation at the biofilm−fluid interface drives pore-scale patterns in mineral precipitation

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Apr 15, 2026 version files 104.07 GB

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Abstract

Microbial oxidation of manganese (Mn) from aqueous Mn(II) to solid-phase Mn(III, IV) minerals catalyzes Mn(II) removal in natural and engineered porous systems. However, little is known about the spatiotemporal evolution of Mn biomineralization in confined spaces that experience simultaneous Mn(II) delivery and Mn oxide precipitation. In this work, we combined time-lapse microscopy, image analysis, and mass spectrometry to quantify the extent and rate of Mn biomineralization by Pseudomonas putida GB-1 in an optically transparent two-dimensional porous medium. We conducted microfluidic experiments in triplicate and collected both optical images (color brightfield and mCherry fluorescence) and effluent samples for each replicate. We also developed a calibration curve using optical microscopy and micro-X-ray fluorescence to convert pixel intensity to Mn oxide mass. Images were analyzed with custom MATLAB (2024b) scripts to quantify total Mn oxide accumulation and the rate of mineral precipitation as a function of time and space. Effluent samples were analyzed with inductively coupled plasma mass spectrometry (ICP-MS) to measure Mn(II) removal. From these data, we found that Mn(II) oxidation initially occurred within biofilms but shifted over time towards the edges of biofilms in contact with pore fluid. Minerals precipitated outside of the initial biofilm footprint due to surface-mediated oxidation of Mn(II) by nascent biogenic Mn oxides, reinforcing a gradient in mineral accumulation from the Mn(II) source near the reactor inlet to the outlet. The rate of mineral precipitation outside the biofilm footprint surpassed the rate of mineral accumulation inside biofilms within six hours and accounted for two-thirds of the total Mn oxide mass in the pore space at the end of the experiment. This work advances a mechanistic understanding of coupled biotic and abiotic Mn oxidation in porous environments, while providing a novel platform to quantify microbe-mineral-fluid interactions.