Dissolution rate of quartz in lead and sodium electrolyte solutions between 25 and 300°C: Effect of the nature of surface complexes and reaction affinity
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The coordination chemistry of weathering: III. A generalization on the dissolution rates of minerals
The 12 references without a DOI — listed, not checked
no DOI — not checkedMultiple activated complex dissolution of oxides: modeling of the proton promoted dissolution of strained and unstrained quartz
no DOI — not checkedDissolution and precipitation kinetics of kaolinite as a junction of chemical allinity (T= 150°C, pH = 2 and 7.8)
no DOI — not checkedQuartz dissolution kinetics in electrolyte solutions from 25 to 300°C
no DOI — not checkedThe influence of pH on the hydrothermal dissolution kinetics of quartz in solutions of electrolyte and transition metals
no DOI — not checkedThe role of salts in the dissolution of powdered quartz
no DOI — not checkedTransition State Theory
no DOI — not checkedAb Initio quantum-mechenical calculations of surface reactions. A new era?
no DOI — not checkedThe dissolution rate of albite as a function of chemical affinity and the stoichiometry of activated complexes in aluminosilicate dissolution reactions
no DOI — not checkedModeling of the dissolution of strained and unstrained multiple oxides: The surface speciation approach
no DOI — not checkedDetermination of reactive silicate
no DOI — not checkedCalculation of chemical equilibrium between aqueous solution and minerals: The EQ3/6 software package
no DOI — not checkedRate control of weathering of silicate minerals at room temperature and pressure
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