Rates of mineral dissolution under CO2 storage conditions
Abstract
Evaluating the potential of a sedimentary basin reservoir to securely store CO2 benefits from a comprehensive understanding of the geochemical reactions that take place once CO2 is injected into a formation. In particular, models that predict the transport and reaction of CO2 within a reservoir require a definition of the types of reactions affected by enhanced levels of CO2 and how the kinetics of these reactions will affect a heterogeneous mineralogy and formation waters within a reservoir over time. In this review we evaluate rate models used to describe mineral dissolution kinetics and compare the range in values reported for the kinetic parameters used to describe the reactivity of various minerals relevant to mainly siliciclastic reservoirs. Parameters that have a significant impact on model results include the reactive surface area of a mineral, the apparent activation energies used to extrapolate reaction rates to the temperatures of potential storage reservoirs (c. 50–125 °C) and the in-situ pH of formation waters with elevated concentrations of dissolved CO2. The variation in reported values for these parameters can lead to predicted rates that span many orders of magnitude for a given mineral. Despite these uncertainties recent success with geochemical models has been made bymore »
- Authors:
-
- Cooperative Research Centre for Greenhouse Gas Technologies (Australia); Univ. of Melbourne (Australia)
- Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
- Publication Date:
- Research Org.:
- Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
- Sponsoring Org.:
- USDOE Office of Fossil Energy (FE); USDOE Office of Fossil Energy and Carbon Management (FECM)
- OSTI Identifier:
- 1812142
- Alternate Identifier(s):
- OSTI ID: 1249673
- Report Number(s):
- LLNL-JRNL-700437
Journal ID: ISSN 0009-2541; 828508
- Grant/Contract Number:
- AC52-07NA27344
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Chemical Geology
- Additional Journal Information:
- Journal Volume: 399; Journal Issue: N/A; Journal ID: ISSN 0009-2541
- Publisher:
- Elsevier
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; 37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; Mineral dissolution rates; Geochemical modelling; CO2 storage
Citation Formats
Black, Jay R., Carroll, Susan A., and Haese, Ralf R. Rates of mineral dissolution under CO2 storage conditions. United States: N. p., 2015.
Web. doi:10.1016/j.chemgeo.2014.09.020.
Black, Jay R., Carroll, Susan A., & Haese, Ralf R. Rates of mineral dissolution under CO2 storage conditions. United States. https://doi.org/10.1016/j.chemgeo.2014.09.020
Black, Jay R., Carroll, Susan A., and Haese, Ralf R. Wed .
"Rates of mineral dissolution under CO2 storage conditions". United States. https://doi.org/10.1016/j.chemgeo.2014.09.020. https://www.osti.gov/servlets/purl/1812142.
@article{osti_1812142,
title = {Rates of mineral dissolution under CO2 storage conditions},
author = {Black, Jay R. and Carroll, Susan A. and Haese, Ralf R.},
abstractNote = {Evaluating the potential of a sedimentary basin reservoir to securely store CO2 benefits from a comprehensive understanding of the geochemical reactions that take place once CO2 is injected into a formation. In particular, models that predict the transport and reaction of CO2 within a reservoir require a definition of the types of reactions affected by enhanced levels of CO2 and how the kinetics of these reactions will affect a heterogeneous mineralogy and formation waters within a reservoir over time. In this review we evaluate rate models used to describe mineral dissolution kinetics and compare the range in values reported for the kinetic parameters used to describe the reactivity of various minerals relevant to mainly siliciclastic reservoirs. Parameters that have a significant impact on model results include the reactive surface area of a mineral, the apparent activation energies used to extrapolate reaction rates to the temperatures of potential storage reservoirs (c. 50–125 °C) and the in-situ pH of formation waters with elevated concentrations of dissolved CO2. The variation in reported values for these parameters can lead to predicted rates that span many orders of magnitude for a given mineral. Despite these uncertainties recent success with geochemical models has been made by applying a Monte Carlo approach to optimise the kinetic parameters for minerals where robust thermodynamic and kinetic data do not exist.},
doi = {10.1016/j.chemgeo.2014.09.020},
journal = {Chemical Geology},
number = N/A,
volume = 399,
place = {United States},
year = {Wed Apr 01 00:00:00 EDT 2015},
month = {Wed Apr 01 00:00:00 EDT 2015}
}
Web of Science
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