Transformation of meta-stable calcium silicate hydrates to tobermorite: reaction kinetics and molecular structure from XRD and NMR spectroscopy

Houston, Jacqueline R.; Maxwell, Robert S.; Carroll, Susan A.

doi:10.1186/1467-4866-10-1

Transformation of meta-stable calcium silicate hydrates to tobermorite: reaction kinetics and molecular structure from XRD and NMR spectroscopy

Journal Article · Wed Jan 14 00:00:00 EST 2009 · Geochemical Transactions

DOI:https://doi.org/10.1186/1467-4866-10-1· OSTI ID:1626251

Houston, Jacqueline R. ^[1]; Maxwell, Robert S. ^[2]; Carroll, Susan A. ^[2]

Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States). Chemistry, Materials, Earth, and Life Sciences Directorate; DOE/OSTI
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States). Chemistry, Materials, Earth, and Life Sciences Directorate

Understanding the integrity of well-bore systems that are lined with Portland-based cements is critical to the successful storage of sequestered CO₂ in gas and oil reservoirs. As a first step, we investigate reaction rates and mechanistic pathways for cement mineral growth in the absence of CO₂ by coupling water chemistry with XRD and NMR spectroscopic data. We find that semicrystalline calcium (alumino-)silicate hydrate (Al-CSH) forms as a precursor solid to the cement mineral tobermorite. Rate constants for tobermorite growth were found to be k = 0.6 (± 0.1) × 10^-5 s^-1 for a solution:solid of 10:1 and 1.6 (± 0.8) × 10^-4 s^-1 for a solution:solid of 5:1 (batch mode; T = 150°C). This data indicates that reaction rates for tobermorite growth are faster when the solution volume is reduced by half, suggesting that rates are dependent on solution saturation and that the Gibbs free energy is the reaction driver. However, calculated solution saturation indexes for Al-CSH and tobermorite differ by less than one log unit, which is within the measured uncertainty. Based on this data, we consider both heterogeneous nucleation as the thermodynamic driver and internal restructuring as possible mechanistic pathways for growth. We also use NMR spectroscopy to characterize the site symmetry and bonding environment of Al and Si in a reacted tobermorite sample. We find two ^[4]Al coordination structures at δ_iso = 59.9 ppm and 66.3 ppm with quadrupolar product parameters (P_Q) of 0.21 MHz and 0.10 MHz (± 0.08) from ²⁷Al 3Q-MAS NMR and speculate on the Al occupancy of framework sites by probing the protonation environment of Al metal centers using ²⁷Al{¹H}CP-MAS NMR.

View Accepted Manuscript (DOE)

Research Organization:: Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences & Biosciences Division

Grant/Contract Number:: AC52-07NA27344

OSTI ID:: 1626251

Journal Information:: Geochemical Transactions, Journal Name: Geochemical Transactions Journal Issue: 1 Vol. 10; ISSN 1467-4866

Publisher:: American Chemical Society, Geochemistry Div.Copyright Statement

Country of Publication:: United States

Language:: English

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Transformation of meta-stable calcium silicate hydrates to tobermorite: reaction kinetics and molecular structure from XRD and NMR spectroscopy

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