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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

https://doi.org/10.1016/0016-7037(94)90487-1
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33/33 checkable references clean · checked 2026-07-22

Every reference with a DOI in the deposited reference list resolved to a known work in Crossref or DataCite at the dated check, and none carried a retraction, withdrawal, or removal notice.

12 without a DOI — not checked. A reference deposited without a DOI is never matched by title or guessed at; it stays outside the checked set, and this line discloses that.

The 33 checked references that resolve
resolves10.2475/ajs.282.3.237
Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions; I, Theoretical considerations
resolves10.1016/0016-7037(85)90228-5
Dissolution kinetics of chrysotile at pH 7 to 10
resolves10.1016/0016-7037(91)90023-X
Quartz dissolution in organic-rich aqueous systems
resolves10.1016/0016-7037(88)90222-0
The dissolution of quartz in dilute aqueous solutions of organic acids at 25°C
resolves10.1038/331431a0
Role of surface speciation in the low-temperature dissolution of minerals
resolves10.1016/0016-7037(90)90318-F
The effect of dislocation density on the dissolution rate of quartz
resolves10.1021/j100567a012
Consistency between kinetics and thermodynamics
resolves10.1016/0009-2541(90)90084-K
Kinetics of quartz dissolution at low temperatures
resolves10.1016/0009-2541(93)90123-Z
Free energy dependence of albite dissolution kinetics at 80°C and pH 8.8
resolves10.1080/14786435608238124
XLV. On the dislocation theory of evaporation of crystals
resolves10.1016/0021-9797(78)90217-5
Surface ionization and complexation at the oxide/water interface II. Surface properties of amorphous iron oxyhydroxide and adsorption of metal ions
resolves10.1016/0016-7037(90)90431-J
Kinetics of quartz dissolution in electrolyte solutions using a hydrothermal mixed flow reactor
resolves10.1016/0016-7037(92)90257-J
Dissolution kinetics of quartz in sodium chloride solutions: Analysis of existing data and a rate model for 25°C
resolves10.1016/0016-7037(86)90243-7
The coordination chemistry of weathering: I. Dissolution kinetics of δ-Al2O3 and BeO
resolves10.1016/0021-9797(89)90012-X
Temperature dependence of the electrical double layer on oxides: Rutile and hematite
resolves10.1016/0009-2541(89)90057-0
Multisite surface reaction versus transport control during the hydrolysis of a complex oxide
resolves10.1016/0021-9797(87)90078-6
Modeling ionic strength effects on cation adsorption at hydrous oxide/solution interfaces
resolves10.1029/JB080i014p01885
Elastic stresses and self-energies of dislocations of arbitrary orientation in anisotropic media: Olivine, orthopyroxene, calcite, and quartz
resolves10.1016/0021-9797(90)90084-2
Multiple activated complex dissolution of metal (hydr) oxides: A thermodynamic approach applied to quartz
resolves10.1039/jr9550000773
The chemistry of silica surfaces
resolves10.1016/0021-9797(84)90457-0
A thermodynamic description of the double layer surrounding hydrous oxides
resolves10.1016/0016-7037(85)90003-1
Mg2+ removal in the system Mg2+—amorphous SiO2—H2O by adsorption and Mg-hydroxysilicate precipitation
resolves10.1016/0016-7037(88)90055-5
The dissolution kinetics of quartz as a function of pH and time at 70°C
resolves10.1016/0016-7037(86)90088-8
Surface chemistry, etch pits and mineral-water reactions
resolves10.1016/0016-7037(92)90291-P
Dissolution and precipitation kinetics of gibbsite at 80°C and pH 3: The dependence on solution saturation state
resolves10.2475/ajs.291.7.649
Dissolution and precipitation kinetics of kaolinite at 80 degrees C and pH 3; the dependence on solution saturation state
resolves10.1029/JB089iB06p03997
Surface and interfacial free energies of quartz
resolves10.1007/BF00650397
Ionization constants of aqueous ammonia from 25 to 250�C and to 2000 bar
resolves10.1016/0016-7037(80)90220-3
The kinetics of silica-water reactions
resolves10.1016/0016-7037(87)90177-3
Dissolution of quartz into dilute alkaline solutions at 90°C: A kinetic study
resolves10.1029/RG028i001p00053
Coordination chemistry of weathering: Kinetics of the surface‐controlled dissolution of oxide minerals
resolves10.1021/j100840a017
THE SOLUBILITY OF QUARTZ
resolves10.1016/0016-7037(88)90178-0
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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