Transformation of meta-stable calcium silicate hydrates to tobermorite: reaction kinetics and molecular structure from XRD and NMR spectroscopy
Understanding the integrity of well-bore systems that are lined with Portland-based cements is critical to the successful storage of sequestered CO 2 in gas and oil reservoirs. As a first step, we investigate reaction rates and mechanistic pathways for cement mineral growth in the absence of CO 2 by...
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Published in: | Geochemical transactions GT Vol. 10; no. 1; p. 1 |
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Main Authors: | , , |
Format: | Journal Article |
Language: | English |
Published: |
Cham
Springer International Publishing
14-01-2009
BioMed Central Ltd American Chemical Society, Geochemistry Div BioMed Central BMC |
Subjects: | |
Online Access: | Get full text |
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Summary: | Understanding the integrity of well-bore systems that are lined with Portland-based cements is critical to the successful storage of sequestered CO
2
in gas and oil reservoirs. As a first step, we investigate reaction rates and mechanistic pathways for cement mineral growth in the absence of CO
2
by coupling water chemistry with XRD and NMR spectroscopic data. We find that semi-crystalline 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
27
Al 3Q-MAS NMR and speculate on the Al occupancy of framework sites by probing the protonation environment of Al metal centers using
27
Al{
1
H}CP-MAS NMR. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 AC52-07NA27344 USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences & Biosciences Division |
ISSN: | 1467-4866 1467-4866 |
DOI: | 10.1186/1467-4866-10-1 |