Biogenic hydrogen production from residual oil in geological carbon storage sites

We found that the combined supply of protein-rich matter and supercritical CO₂ to petroleum produced water (PW) stimulates the biogenic production of H₂ from dissolved oil hydrocarbons by indigenous microbial communities of oil reservoirs. Our experimental results support the hypothesis that a decrease in pH to acidic levels due to the dissolution of supercritical CO₂ into the aqueous phase and the availability of protein-rich matter, favors the activity of H₂-producing microbial communities over the activity of H₂-using microbial communities. To determine where, when, and how much H₂ could be produced in a depleted oil reservoir co-injected with CO₂ and PW supplied with protein-rich matter, we simulated the biogenic production of H₂ for the Morrow B sandstone reservoir. Our simulation results indicate that 365 – 1925 kg of H₂ could be produced after 100 days of CO₂ and PW co-injection (1.5 kg-CO₂/1.5 kg-PW – 7.5 kg-CO₂/7.5 kg-PW) into a single well of radial flow of uniform porosity and permeability, and that sandstone reservoirs are more suitable than carbonate reservoirs to produce H₂ by the proposed stimulation method. Simulations were conducted using our own TOUGHREACT module called CO2Bio. CO2Bio simulates the multiphase bio-geochemical reactive transport of CO₂-CH₄-H₂-H₂S mixture gases in geological carbon storage sites. To determine the effect of permeability heterogeneity on the biogenic production of H₂ by the proposed stimulation method, we incorporated permeability heterogeneity into the model consisting of a single well of radial flow. This task was achieved by measuring the permeability of four core samples of the Morrow B sandstone reservoir, and by applying a kriging geostatistical interpolation method. Simulation results indicate that heterogeneity reduces the amount of H₂ production by the proposed stimulation method, and that larger amounts of H₂ are produced in zones of high permeability than in zones of low permeability. An additional simulation was conducted placing multiple wells across the whole reservoir. After 100 days of injecting 5 kg-CO₂/5 kg-PW – 10 kg-CO₂/10 kg-PW, H₂ productions was 3,712 kg – 13,489 kg of H₂. Overall, the results indicate that biogenic H₂ production in geological carbon storage sites is feasible and a function of petrophysical, geochemical, and microbiological factors.

Publication Details

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SHAREOK (University of Oklahoma; Oklahoma State University; Central Oklahoma University)
Published
2024-12-01
Primary Topic
CO2 Sequestration and Geologic Interactions
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article

Biogenic hydrogen production from residual oil in geological carbon storage sites

SHAREOK (University of Oklahoma; Oklahoma State University; Central Oklahoma University)
CO2 Sequestration and Geologic Interactions
article

Biogenic hydrogen production from residual oil in geological carbon storage sites

article en

Abstract

We found that the combined supply of protein-rich matter and supercritical CO₂ to petroleum produced water (PW) stimulates the biogenic production of H₂ from dissolved oil hydrocarbons by indigenous microbial communities of oil reservoirs. Our experimental results support the hypothesis that a decrease in pH to acidic levels due to the dissolution of supercritical CO₂ into the aqueous phase and the availability of protein-rich matter, favors the activity of H₂-producing microbial communities over the activity of H₂-using microbial communities. To determine where, when, and how much H₂ could be produced in a depleted oil reservoir co-injected with CO₂ and PW supplied with protein-rich matter, we simulated the biogenic production of H₂ for the Morrow B sandstone reservoir. Our simulation results indicate that 365 – 1925 kg of H₂ could be produced after 100 days of CO₂ and PW co-injection (1.5 kg-CO₂/1.5 kg-PW – 7.5 kg-CO₂/7.5 kg-PW) into a single well of radial flow of uniform porosity and permeability, and that sandstone reservoirs are more suitable than carbonate reservoirs to produce H₂ by the proposed stimulation method. Simulations were conducted using our own TOUGHREACT module called CO2Bio. CO2Bio simulates the multiphase bio-geochemical reactive transport of CO₂-CH₄-H₂-H₂S mixture gases in geological carbon storage sites. To determine the effect of permeability heterogeneity on the biogenic production of H₂ by the proposed stimulation method, we incorporated permeability heterogeneity into the model consisting of a single well of radial flow. This task was achieved by measuring the permeability of four core samples of the Morrow B sandstone reservoir, and by applying a kriging geostatistical interpolation method. Simulation results indicate that heterogeneity reduces the amount of H₂ production by the proposed stimulation method, and that larger amounts of H₂ are produced in zones of high permeability than in zones of low permeability. An additional simulation was conducted placing multiple wells across the whole reservoir. After 100 days of injecting 5 kg-CO₂/5 kg-PW – 10 kg-CO₂/10 kg-PW, H₂ productions was 3,712 kg – 13,489 kg of H₂. Overall, the results indicate that biogenic H₂ production in geological carbon storage sites is feasible and a function of petrophysical, geochemical, and microbiological factors.

SHAREOK (University of Oklahoma; Oklahoma State University; Central Oklahoma University)
Clean water and sanitation
Openalex Percentile: Top 58%
CO2 Sequestration and Geologic Interactions
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Biogenic hydrogen production from residual oil in geological carbon storage sites · SHAREOK (University of Oklahoma; Oklahoma State University; Central Oklahoma University) (2024) | TGRS Research Map | TGRS