Metal oxide minerals play a critical role in biogeochemical cycling1. Manganese (Mn) and iron (Fe) oxides are negatively charged at circumneutral pH and readily sorb cationic metals2,3,4,5,6,7,8, regulating micronutrient availability and contaminant mobility in the rhizosphere and hyporheic zone. These minerals influence the stability and degradation of organic matter9,10,11,12, dictating carbon uptake by plants and soil microbes. In engineered systems (e.g., water treatment filters, constructed wetlands), metal oxide precipitation is directly leveraged for Mn or Fe removal and remediation of co-occurring contaminants13,14,15,16,17. These metal oxides are identifiable by their characteristic colors, which range from ochre to dark brown to black18,19.
The precipitation of metal oxides is commonly facilitated by microorganisms in a process known as biomineralization20,21,22. Numerous Mn-oxidizing bacteria and fungi synthesize multicopper oxidases and peroxidases that catalyze electron transfer from Mn(II) to Mn(III) and Mn(IV) under aerobic conditions, resulting in the precipitation of birnessite-like Mn(III, IV) oxide minerals2,23,24. Additionally, diverse Fe-oxidizing bacteria enzymatically oxidize Fe(II) to Fe(III) in circumneutral or acidic environments limited in oxygen, producing Fe(II, III) (oxyhydr)oxides, including ferrihydrite and magnetite25,26,27,28. These biogenic minerals precipitate adjacent to cell surfaces and accumulate on extracellular polymers, sheaths, and other cellular structures, forming microbe-mineral assemblages2,23,25,27,29,30.
Despite the ubiquity of Mn and Fe biomineralization in complex environments, pore-scale insights are lacking. Pore spaces are structurally heterogeneous, exhibiting preferential fluid flow and nonuniform reactant transport that dictate the distribution of biogeochemical reactions31,32,33,34,35. Further, microbial activity may generate local geochemical gradients that promote or limit biomineralization, while fluctuations in pore fluid chemistry (e.g., pH, dissolved oxygen, redox potential) may enhance mineral precipitation or facilitate dissolution34,35. Studies of Mn and Fe biomineralization typically rely either on well-mixed batch conditions30,36,37,38,39,40 or columns41,42,43,44 to quantify oxidation kinetics or characterize biomineral precipitates. However, batch experiments lack the spatial heterogeneity inherent to porous systems. Columns containing packed granular media provide relevant physical architecture but are limited in their utility because they require destructive sampling at static timepoints, which halts the experiment progression and prevents unperturbed pore-scale observations. Therefore, new experimental approaches are needed to investigate the microbial precipitation of metal oxides in porous media.
Microfluidic systems are a tool to study biogeochemical reactions in situ and in real time. Microfluidic reactors can be fabricated rapidly and at low cost with reproducible and customizable geometries that simulate natural or idealized porous media45. The resulting devices are optically transparent, facilitating non-destructive visualization and quantification of pore-scale processes, including biofilm formation46,47,48,49, hotspot development50,51, abiotic metal precipitation52,53, and calcite biomineralization34,54,55,56. Additionally, microfluidic systems allow users to control and systematically vary boundary conditions, including metal concentration, presence or absence of dissolved oxygen, and fluid flow rate. Finally, depending on the reactor substrate material, direct measurements of microbe-mineral-fluid interactions can be acquired using X-ray, Raman, or infrared spectroscopy57. The development of such a microfluidics-based platform to study the microbial precipitation of metal oxides thus provides an avenue for novel research on the formation and reactivity of Mn or Fe mineral phases that drive carbon, nutrient, and contaminant cycling in porous environments.
This work uses Mn biomineralization as a case study to quantify the microbial precipitation of metal oxides in a dynamic porous environment. The following protocol demonstrates how to fabricate and inoculate a microfluidic reactor with Pseudomonas putida GB-1, a model bacterium known to oxidize Mn(II) to Mn(III, IV) at its stationary phase of growth58,59. Using a pressure-based flow control system, nutrient-rich growth medium and minimal salt solution are sequentially injected to promote biofilm formation and induce Mn oxide precipitation, respectively. High-resolution color brightfield images of the microfluidic pore space are collected at regular time intervals, capturing the color contrast between P. putida GB-1 biofilms and accumulating Mn oxides. At the end of each experiment, all Mn oxides contained within the reactor are digested, and the total mass is measured with inductively coupled plasma mass spectrometry (ICP-MS). The rate of Mn oxide precipitation is estimated as a function of time by integrating these endpoint mass measurements with an image subtraction algorithm. This workflow can be readily adapted to investigate other organisms or metal oxide precipitation processes under a variety of environmental conditions.