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    Determining the Complete Stability of Calcite Kink Sites: Real vs Ideal

    96245.pdf (7.364Mb)
    Access Status
    Open access
    Authors
    Armstrong, Blake I.
    Silvestri, Alessandro
    De La Pierre, Marco
    Raiteri, Paolo
    Gale, Julian D.
    Date
    2023
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Armstrong, B.I. and Silvestri, A. and De La Pierre, M. and Raiteri, P. and Gale, J.D. 2023. Determining the Complete Stability of Calcite Kink Sites: Real vs Ideal. Journal of Physical Chemistry C. 127 (28): pp. 13958-13968.
    Source Title
    Journal of Physical Chemistry C
    DOI
    10.1021/acs.jpcc.3c02864
    ISSN
    1932-7447
    Faculty
    Faculty of Science and Engineering
    School
    School of Molecular and Life Sciences (MLS)
    Funding and Sponsorship
    http://purl.org/au-research/grants/arc/FL180100087
    Remarks

    This document is the Accepted Manuscript version of a Published Work that appeared in final form in The Journal of Physical Chemistry C, copyright © American Chemical Society, after peer review and technical editing by the publisher. To access the final edited and published work see https://pubs.acs.org/doi/10.1021/acs.jpcc.3c02864.

    URI
    http://hdl.handle.net/20.500.11937/96481
    Collection
    • Curtin Research Publications
    Abstract

    Kink sites play a pivotal role in the growth and dissolution of materials at the solid-liquid interface. Despite this, little is known about the thermodynamic stability of such sites. Calcium carbonate, in the form of calcite, is one of the most abundant biominerals and a natural means of carbon sequestration in the environment. Here, we present a complete determination of the standard free energies for all 16 individual kink sites for the significant case of the calcite (101̅4)-water interface using both alchemical- and pathway-based simulation techniques. The results reveal the importance of distinguishing between real and ideal ion-binding free energies at surfaces, especially for calcite-water, where the interfacial potential can alter values by more than 100 kJ/mol per site. Individual kink site stabilities are found to show variations in excess of 60 kJ/mol, which can help explain the observed differences in growth rates between the two distinct steps of calcite.

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