Trace metal source terms in carbon sequestration environments

Athanasios Karamalidis, Sharon G. Torres, J. Alexandra Hakala, Hongbo Shao, Kirk J. Cantrell, Susan Carroll

Research output: Contribution to journalArticle

37 Citations (Scopus)

Abstract

Carbon dioxide sequestration in deep saline and depleted oil geologic formations is feasible and promising; however, possible CO2 or CO2-saturated brine leakage to overlying aquifers may pose environmental and health impacts. The purpose of this study was to experimentally define a range of concentrations that can be used as the trace element source term for reservoirs and leakage pathways in risk simulations. Storage source terms for trace metals are needed to evaluate the impact of brines leaking into overlying drinking water aquifers. The trace metal release was measured from cements and sandstones, shales, carbonates, evaporites, and basalts from the Frio, In Salah, Illinois Basin, Decatur, Lower Tuscaloosa, Weyburn-Midale, Bass Islands, and Grand Ronde carbon sequestration geologic formations. Trace metal dissolution was tracked by measuring solution concentrations over time under conditions (e.g., pressures, temperatures, and initial brine compositions) specific to the sequestration projects. Existing metrics for maximum contaminant levels (MCLs) for drinking water as defined by the U.S. Environmental Protection Agency (U.S. EPA) were used to categorize the relative significance of metal concentration changes in storage environments because of the presence of CO2. Results indicate that Cr and Pb released from sandstone reservoir and shale cap rocks exceed the MCLs by an order of magnitude, while Cd and Cu were at or below drinking water thresholds. In carbonate reservoirs As exceeds the MCLs by an order of magnitude, while Cd, Cu, and Pb were at or below drinking water standards. Results from this study can be used as a reasonable estimate of the trace element source term for reservoirs and leakage pathways in risk simulations to further evaluate the impact of leakage on groundwater quality.

Original languageEnglish (US)
Pages (from-to)322-329
Number of pages8
JournalEnvironmental Science and Technology
Volume47
Issue number1
DOIs
StatePublished - Jan 2 2013

Fingerprint

Drinking Water
carbon sequestration
trace metal
leakage
Carbon
drinking water
Carbonates
Trace Elements
Impurities
Sandstone
Aquifers
brine
pollutant
sandstone
trace element
aquifer
carbonate
Brines
cap rock
Environmental Protection Agency

All Science Journal Classification (ASJC) codes

  • Chemistry(all)
  • Environmental Chemistry

Cite this

Karamalidis, A., Torres, S. G., Hakala, J. A., Shao, H., Cantrell, K. J., & Carroll, S. (2013). Trace metal source terms in carbon sequestration environments. Environmental Science and Technology, 47(1), 322-329. https://doi.org/10.1021/es304832m
Karamalidis, Athanasios ; Torres, Sharon G. ; Hakala, J. Alexandra ; Shao, Hongbo ; Cantrell, Kirk J. ; Carroll, Susan. / Trace metal source terms in carbon sequestration environments. In: Environmental Science and Technology. 2013 ; Vol. 47, No. 1. pp. 322-329.
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Karamalidis, A, Torres, SG, Hakala, JA, Shao, H, Cantrell, KJ & Carroll, S 2013, 'Trace metal source terms in carbon sequestration environments', Environmental Science and Technology, vol. 47, no. 1, pp. 322-329. https://doi.org/10.1021/es304832m

Trace metal source terms in carbon sequestration environments. / Karamalidis, Athanasios; Torres, Sharon G.; Hakala, J. Alexandra; Shao, Hongbo; Cantrell, Kirk J.; Carroll, Susan.

In: Environmental Science and Technology, Vol. 47, No. 1, 02.01.2013, p. 322-329.

Research output: Contribution to journalArticle

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