Pore-scale simulation of microbial growth using a genome-scale metabolic model: Implications for Darcy-scale reactive transport

•We model microbially-mediated iron reduction at the pore scale.•We simulate microbial metabolism using a genome-scale modeling approach.•We compare the genome-scale and Monod kinetic rate models.•We examine effects of pore-scale mixing on effective reaction rates.•Diffusion limitations on pore-scal...

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Bibliographic Details
Published in:Advances in water resources 2013-09, Vol.59, p.256-270
Main Authors: Tartakovsky, G.D., Tartakovsky, A.M., Scheibe, T.D., Fang, Y., Mahadevan, R., Lovley, D.R.
Format: Article
Language:English
Subjects:
Biogeochemistry
Computer simulation
Earth sciences
Earth, ocean, space
Exact sciences and technology
Fluxes
Genome-scale model
Geobacter
Geobacter sulfurreducens
Hydrology
Hydrology. Hydrogeology
Iron
Mathematical models
Metal reduction
Microorganisms
Navier-Stokes equations
Nutrients
Pore-scale
Scale (ratio)
Simulation
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Summary:•We model microbially-mediated iron reduction at the pore scale.•We simulate microbial metabolism using a genome-scale modeling approach.•We compare the genome-scale and Monod kinetic rate models.•We examine effects of pore-scale mixing on effective reaction rates.•Diffusion limitations on pore-scale mixing reduce effective reaction rates. Recent advances in microbiology have enabled the quantitative simulation of microbial metabolism and growth based on genome-scale characterization of metabolic pathways and fluxes. We have incorporated a genome-scale metabolic model of the iron-reducing bacteria Geobacter sulfurreducens into a pore-scale simulation of microbial growth based on coupling of iron reduction to oxidation of a soluble electron donor (acetate). In our model, fluid flow and solute transport is governed by a combination of the Navier–Stokes and advection–diffusion–reaction equations. Microbial growth occurs only on the surface of soil grains where solid-phase mineral iron oxides are available. Mass fluxes of chemical species associated with microbial growth are described by the genome-scale microbial model, implemented using a constraint-based metabolic model, and provide the Robin-type boundary condition for the advection–diffusion equation at soil grain surfaces. Conventional models of microbially-mediated subsurface reactions use a lumped reaction model that does not consider individual microbial reaction pathways, and describe reactions rates using empirically-derived rate formulations such as the Monod-type kinetics. We have used our pore-scale model to explore the relationship between genome-scale metabolic models and Monod-type formulations, and to assess the manifestation of pore-scale variability (microenvironments) in terms of apparent Darcy-scale microbial reaction rates. The genome-scale model predicted lower biomass yield, and different stoichiometry for iron consumption, in comparison to prior Monod formulations based on energetics considerations. We were able to fit an equivalent Monod model, by modifying the reaction stoichiometry and biomass yield coefficient, that could effectively match results of the genome-scale simulation of microbial behaviors under excess nutrient conditions, but predictions of the fitted Monod model deviated from those of the genome-scale model under conditions in which one or more nutrients were limiting. The fitted Monod kinetic model was also applied at the Darcy scale; that is, to simulate average rea
ISSN:0309-1708
1872-9657
DOI:10.1016/j.advwatres.2013.05.007