Numerical modeling and simulation of microbial methanogenesis in geological CO2 storage sites

Abstract

Abstract A numerical model was developed to assess the feasibility of microbial CH 4 generation in geological CO 2 storage sites. The model accounts for water-rock geochemical reactions, microbial competition between methanogenic microbes and sulfate reducing bacteria (SRB) for H 2 and acetate, and the effect of pH on the activity of microbes. For the sake of analysis, carbohydrates contained in the stimulating nutrient injected along with CO 2 serves as source for the biogenic formation of H 2 and acetate by H 2 -forming fermentative microbes. Simulation results unveiled that the pH buffering effect of carbonate minerals such as calcite is of outmost importance to push methanogenesis reactions. CO 2 injection into a geological formation containing calcite enhances the biogenic supply of H 2 and acetate by providing near optimum pH conditions for the activity of H 2 -forming fermentative microbes. However, when sulfate in the formation water is present in excesses, hydrogenotrophic and acetotrophic SRB outcompete hydrogenotrophic and acetotrophic methanogenic microbes for H 2 and acetate, respectively. This is reflected by the predominant formation of H 2 S and negligible formation of CH 4 . With calcite in the mineral phase, the activity of SRB and methanogenic microbes is governed by their initial concentrations in the formation water. Without calcite in the mineral phase, injection of CO 2 inhibits the activity of hydrogenotrophic and acetotrophic SRB and methanogenic microbes, but not the activity of H 2 -forming fermentative microbes. The activity of H 2 -forming fermentative microbes is not conditioned to the presence of calcite in the mineral phase as their optimum pH falls within the acidic range that results from the injection of CO 2 . Without sufficient amounts of sulfate in the formation water to support the activity of SRB, injection of CO 2 into a geological formation containing calcite favors the biogenic formation of CH 4 via the reduction pathway of CO 2 with H 2 , whereas without CO 2 injection methanogenesis via acetate fermentation is favored. Methanogenesis in geological CO 2 storage sites is possible under controlled CO 2 and stimulating organic nutrients injection. Oil reservoirs containing calcite in the mineral phase and low concentrations of sulfate in the formation water are most suitable for microbial methanogenesis from CO 2 in geological CO 2 storage sites.