4.8 Article

In Situ Natural Abundance 17O and 25Mg NMR Investigation of Aqueous Mg(OH)2 Dissolution in the Presence of Supercritical CO2

Journal

ENVIRONMENTAL SCIENCE & TECHNOLOGY
Volume 50, Issue 22, Pages 12373-12384

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acs.est.6b03443

Keywords

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Funding

  1. Geosciences Research Program in the U.S. Department of Energy, Office of Basic Energy Sciences, Chemical Sciences, Geosciences & Biosciences Division, through its Geosciences program at Pacific Northwest National Laboratory (PNNL)
  2. U.S. Department of Energy's Office of Biological and Environmental Research
  3. Robert Ramsay Chair Fund of The University of Alabama

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We report an in situ high-pressure NMR capability that permits natural abundance O-17 and Mg-25 NMR characterization of dissolved species in aqueous solution and in the presence of supercritical CO2 fluid (scCO(2)). The dissolution of Mg(OH)(2) (brucite) in a multiphase water/scCO(2) fluid at 90 atm pressure and 50 degrees C was studied in situ, with relevance to geological carbon sequestration. O-17 NMR spectra allowed identification and distinction of various fluid species including dissolved CO2 in the H2O-rich phase, scCO(2), aqueous H2O, and HCO3. The widely separated spectral peaks for various species can all be observed both dynamically and quantitatively at concentrations as low as 20 mM. Measurement of the concentrations of these individual species also allows an in situ estimate of the hydrogen ion concentration, or pCH values, of the reacting solutions. The concentration of Mg2+ can be observed by natural abundance Mg-25 NMR at a concentration as low as 10 mM. Quantum chemistry calculations of the NMR chemical shifts on cluster models aided in the interpretation of the experimental results. Evidence for the formation of polymeric Mg2+ clusters at high concentrations in the H2O-rich phase, a possible critical step needed for magnesium carbonate formation, was found.

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