An SN2 reaction mechanism for hydrolysis of siloxane linkages and the implications for dissolution of quartz

Density functional theory calculations were performed on an extended silicate molecular cluster to test the hypothesis that inclusion of Cl<sup>-</sup> to charge-balance protonation of bridging O atoms in siloxane bridges, and H<sub>2</sub>O attack via an S<sub>N</sub>2 mechanism, could explain the observed activation energy of quartz dissolution under acidic conditions. The results are consistent with this hypothesis and help explain the observed solution pH and salt-dependence of quartz dissolution rates.

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Publication Details

Journal
Scientific Reports
Published
2025-11-27
DOI
https://doi.org/10.1038/s41598-025-26643-4
Citations
1
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
0.80

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article

An SN2 reaction mechanism for hydrolysis of siloxane linkages and the implications for dissolution of quartz

Heath D. Watts, James D. Kubicki
1 citations
Scientific Reports
CO2 Sequestration and Geologic Interactions
0.80
article

An SN2 reaction mechanism for hydrolysis of siloxane linkages and the implications for dissolution of quartz

Heath D. Watts, James D. Kubicki
article en
1 citations

Abstract

Density functional theory calculations were performed on an extended silicate molecular cluster to test the hypothesis that inclusion of Cl<sup>-</sup> to charge-balance protonation of bridging O atoms in siloxane bridges, and H<sub>2</sub>O attack via an S<sub>N</sub>2 mechanism, could explain the observed activation energy of quartz dissolution under acidic conditions. The results are consistent with this hypothesis and help explain the observed solution pH and salt-dependence of quartz dissolution rates.

Scientific ReportsVol. 15(1)
The University of Texas at El Paso (US)
U.S. Department of Energy, National Energy Research Scientific Computing Center, Office of Science, University of Texas at El Paso
Openalex Percentile: Top 22%
CO2 Sequestration and Geologic Interactions
0.80
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