Research Article| January 01, 2013 Geochemical Monitoring for Potential Environmental Impacts of Geologic Sequestration of CO2 Yousif K. Kharaka; Yousif K. Kharaka Search for other works by this author on: GSW Google Scholar David R. Cole; David R. Cole *Ohio State University, School of Earth Sciences, Columbus, Ohio 43210, U.S.A. Search for other works by this author on: GSW Google Scholar James J. Thordsen; James J. Thordsen Search for other works by this author on: GSW Google Scholar Kathleen D. Gans; Kathleen D. Gans Search for other works by this author on: GSW Google Scholar R. Burt Thomas R. Burt Thomas Search for other works by this author on: GSW Google Scholar Author and Article Information Yousif K. Kharaka David R. Cole *Ohio State University, School of Earth Sciences, Columbus, Ohio 43210, U.S.A. James J. Thordsen Kathleen D. Gans R. Burt Thomas Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © 2013 Mineralogical Society of America Reviews in Mineralogy and Geochemistry (2013) 77 (1): 399–430. https://doi.org/10.2138/rmg.2013.77.11 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Yousif K. Kharaka, David R. Cole, James J. Thordsen, Kathleen D. Gans, R. Burt Thomas; Geochemical Monitoring for Potential Environmental Impacts of Geologic Sequestration of CO2. Reviews in Mineralogy and Geochemistry 2013;; 77 (1): 399–430. doi: https://doi.org/10.2138/rmg.2013.77.11 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Carbon dioxide sequestration is now considered an important component of the portfolio of options for reducing greenhouse gas emissions to stabilize their atmospheric levels at values that would limit global temperature increases to the target of 2 °C by the end of the century (Pacala and Socolow 2004; IPCC 2005, 2007; Benson and Cook 2005; Benson and Cole 2008; IEA 2012; Romanak et al. 2013). Increased anthropogenic emissions of CO2 have raised its atmospheric concentrations from about 280 ppmv during pre-industrial times to ~400 ppmv today, and based on several defined... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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