A new theoretical mineral dissolution rate equation for physicochemical factors

Junghae Choi, Yasuaki Ichikawa, Kazushi Kimoto, Byung Gon Chae

    Research output: Contribution to journalArticlepeer-review

    1 Citation (Scopus)

    Abstract

    The dissolution rate of minerals is affected by not only physical factors but also chemical factors, such as temperature, solid applied stress, pore water pressure and pH. In general, previous studies on mineral dissolution have dissociated these physical and chemical factors. In this paper, we propose a new dissolution rate equation for quartz dissolution that considers the physical and chemical effects of dissolution. Therefore, the reaction rate constant (k), which is the most important factor in the calculation of the reaction rate, was separated into three individual terms: temperature, solid applied stress and pore water pressure. Finally, the theoretical dissolution rate equation is proposed in this study; the equation contains all of the parameters that are related to the dissolution mechanism, such as temperature, solid applied stress at contact zone, pore pressure and pH conditions. To verify the proposed equation, it is compared with the experimental results, which were collected under various physical and chemical conditions; the equation is found to fit the experimental data well.

    Original languageEnglish
    Pages (from-to)549-557
    Number of pages9
    JournalGEOCHEMICAL JOURNAL
    Volume49
    Issue number5
    DOIs
    Publication statusPublished - 2015

    Keywords

    • Adsorption
    • Arrhenius equation
    • Dissolution rate equation
    • Physico-chemical effects
    • Quartz dissolution

    ASJC Scopus subject areas

    • Geophysics
    • Geochemistry and Petrology

    Fingerprint

    Dive into the research topics of 'A new theoretical mineral dissolution rate equation for physicochemical factors'. Together they form a unique fingerprint.

    Cite this