Geochemical Impacts of Carbon Dioxide, Brine, Trace Metal and Organic Leakage into an Unconfined, Oxidizing Limestone Aquifer
An important risk at CO2 storage sites is the potential for groundwater quality impacts. As part of a system to assess the potential for these impacts a geochemical scaling function has been developed, based on a detailed reactive transport model of CO2 and brine leakage into an unconfined, oxidizing carbonate aquifer. Stochastic simulations varying a number of geochemical parameters were used to generate a response surface predicting the volume of aquifer that would be impacted with respect to regulated contaminants. The brine was assumed to contain several trace metals and organic contaminants. Aquifer pH and TDS were influenced by CO2 leakage, while trace metal concentrations were most influenced by the brine concentrations rather than adsorption or desorption on calcite. Organic plume sizes were found to be strongly influenced by biodegradation.
- Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
- Los Alamos National Laboratory, Los Alamos, NM (United States)
- Lawrence Berkeley National Laboratory, Berkeley, CA (United States)
- Publication Date:
- OSTI Identifier:
- Grant/Contract Number:
- Accepted Manuscript
- Journal Name:
- Energy Procedia
- Additional Journal Information:
- Journal Volume: 63; Journal Issue: C; Journal ID: ISSN 1876-6102
- Research Org:
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
- Sponsoring Org:
- Country of Publication:
- United States
- 58 GEOSCIENCES; geochemistry; limestone; trace metals; calcite adsorption; STOMP; reactive transport.
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