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Published byElfreda Haynes Modified over 8 years ago
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Decouple reaction between carbonate and acetate, carbonate and methane, and sulfate and sulfide. Config → Redox Couples… Default setting: all redox reactions are coupled. Decoupling provides for the redox disequilibrium that supplies sulfate reducers and methanogens with energy.
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After decoupling redox pairs, you can add carbon and sulfur species in multiple redox states. Specify domain’s starting fluid composition on the Initial pane Ca-HCO 3 water containing SO 4 2−, pH = 6
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You add reactants and enable redox kinetics on the Reactants pane. add → Simple → Aqueous… → CH3COO− Rate of acetate addition to the aquifer add → Kinetic → Microbial reaction SO 4 −− reducers Methanogens Click to expand
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Identify each microbe with a label and reaction. Microbes can compete for common substrates or carry out separate reactions. Initial biomass Growth yield and decay constant Rate constant, half- saturation constants ATP energy, ATP number Promoting and inhibiting species Specify kinetic, thermodynamic, and growth parameters for each microbe.
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A single inlet fluid flows into the domain for 10 5 years. Define the reaction intervals. Specify what fluids flow into the domain, and when.
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The “inlet” fluid is identical to the Initial fluid The inlet fluid is defined on the Fluids pane
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Domain is 200 km long, divided into 100 nodal blocks Specify domain size and gridding on the Domain pane.
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Set specific discharge or head drop Specify flowrate on the Flow pane.
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Set various mass transport properties on the Medium pane. Run → Go traces the model
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After 10 5 years of metabolism, growth, and decay, two microbiological zones develop in the aquifer.
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Methane accumulates in second zone of the aquifer. SRB dominate where sulfate is abundant.
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