2016
DOI: 10.1016/j.gca.2016.04.046
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The combined effect of temperature and pH on albite dissolution rate under far-from-equilibrium conditions

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Cited by 31 publications
(13 citation statements)
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“…Influences from dissolution of additional silicate minerals such as albite and muscovite likely contributed to the observed differences between the two experiments. This rationale corresponds with the results of previous experiments which have demonstrated that the dissolution rate for both minerals increases with higher temperatures (Gruber et al, 2016;Lammers et al, 2017).…”
Section: Anaerobic Experimentssupporting
confidence: 92%
“…Influences from dissolution of additional silicate minerals such as albite and muscovite likely contributed to the observed differences between the two experiments. This rationale corresponds with the results of previous experiments which have demonstrated that the dissolution rate for both minerals increases with higher temperatures (Gruber et al, 2016;Lammers et al, 2017).…”
Section: Anaerobic Experimentssupporting
confidence: 92%
“…A wealth of information is available on the molecular mechanisms, kinetics, and pH-dependencies of dissolution reactions of carbonate minerals [119][120][121], Fe-(oxy)hydroxides [122,123], and silicate minerals commonly encountered in waste rock [124][125][126]. The kinetics of carbonate dissolution are typically rapid compared to sulfide oxidation (i.e., far from equilibrium [127]), whereas the dissolution of silicates is orders-of-magnitude slower [2].…”
Section: Acid-buffering Reactionsmentioning
confidence: 99%
“…In general, the reaction rates of mineral is increasing with the elevating temperature. While, the mineral solubility will be either increased or decreased when temperature is increasing, which is depending on the thermodynamic properties of the mineral (Griffioen and Appelo, 1993;Gruber et al, 2016). For instance, solubility of silicates increases with the increasing temperature.…”
Section: Introductionmentioning
confidence: 99%