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Dissolution kinetics of quartz in water at high temperatures across the critical state of water
71/71 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.
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The 71 checked references that resolve
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Are quartz dissolution rates proportional to B.E.T. surface areas?
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Mechanisms of classical crystal growth theory explain quartz and silicate dissolution behavior
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Kinetic evidences of the existence of positively charged species at the quartz-aqueous solution interface
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Solubility and near-equilibrium dissolution rates of quartz in dilute NaCl solutions at 398–473K under alkaline conditions
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The effect of dislocation density on the dissolution rate of quartz
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The influence of the alkaline earth cations, magnesium, calcium, and barium on the dissolution kinetics of quartz
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Structure and Hydrogen Bonding in Liquid and Supercritical Aqueous NaCl Solutions at a Pressure of 1000 bar and Temperatures up to 500 °C: A Comprehensive Experimental and Computational Study
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Estimation of the dielectric constant of H2O from experimental solubilities of quartz, and calculation of the thermodynamic properties of aqueous species to 900°C at 2 kb
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Molecular dynamics simulation study of ionic hydration and ion association in dilute and 1 molal aqueous sodium chloride solutions from ambient to supercritical conditions
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A Study of Near‐ and Super‐Critical Fluids Using Diamond Anvil Cell and in‐Situ FT‐IR Spectroscopy
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Hydrothermal study using a new diamond anvil cell with in situ IR spectroscopy under high temperatures and high pressures
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Calculation of the thermodynamic properties of aqueous silica and the solubility of quartz and its polymorphs at high pressures and temperatures
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Summary of the Apparent Standard Partial Molal Gibbs Free Energies of Formation of Aqueous Species, Minerals, and Gases at Pressures 1 to 5000 Bars and Temperatures 25 to 1000 °C
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A method of calculating quartz solubilities in aqueous sodium chloride solutions
resolves10.1016/j.gca.2012.03.006
A thermodynamic model for the system<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" altimg="si32.gif" overflow="scroll"><mml:mrow><mml:msub><mml:mrow><mml:mtext>SiO</mml:mtext></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:ms>–</mml:ms><mml:msub><mml:mrow><mml:mtext>H</mml:mtext></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:mtext>O</mml:mtext></mml:mrow></mml:math>near the upper critical end point based on quartz solubility experiments at 500–1100 °C and 5–20 kbar
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Quartz solubility in H2O-NaCl and H2O-CO2 solutions at deep crust-upper mantle pressures and temperatures: 2–15 kbar and 500–900°C
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Water in the deep Earth: The dielectric constant and the solubilities of quartz and corundum to 60kb and 1200°C
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Solubility modeling of solids in supercritical fluids using the Kirkwood-Buff fluctuation integral with the hard-sphere expansion (RISE) theory
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The Ionization Constant of Water over Wide Ranges of Temperature and Density
The 23 references without a DOI — listed, not checked
no DOI — not checkedThe solubility equilibrium and the rate of solution of quartz in water at high temperatures and high pressures
no DOI — not checkedThe kinetics of the dissolution of crystalline quartz in water at high temperatures and high pressures
no DOI — not checkedThe role of salts in the dissolution of powdered quartz
no DOI — not checkedRate control of weathering of silicate minerals at room temperature and pressure
no DOI — not checked10.1016/j.supflu.2015.02.010_bib0055
no DOI — not checkedCorrelating quartz dissolution kinetics in pure water from 25 to 625°C
no DOI — not checked10.1016/j.supflu.2015.02.010_bib0075
no DOI — not checkedFluids and reactions in extreme conditions of the earth interior
no DOI — not checkedModeling of the dissolution of strained and unstrained multiple oxides: the surface speciation approach
no DOI — not checkedMultiple activated complex dissolution of oxides: modeling of the proton promoted dissolution of strained and unstrained quartz, Sixth meeting of the Europe Union of Geosciences
no DOI — not checkedTransition state theory
no DOI — not checkedSupercritical water, special report
no DOI — not checkedSilica–water interactions
no DOI — not checkedDissolution reaction kinetics of fluorite in flow systems and its surface chemistry
no DOI — not checkedKinetics of mineral–water reactions in hydrothermal flow systems at elevated temperatures and pressures
no DOI — not checkedA numerical criterion for existence of the equilibrium state in an open chemical system
no DOI — not checkedDielectric constant of water discovered to be simple function of density over extreme ranges from 35 to 600°C and to 1200MPa (12000 Atm.), believed universal
no DOI — not checkedAqueous electrolyte ionization over extreme ranges as simple fundamental relation with density and believed universal; sodium chloride ionization from 0 to 1000°C and to 1000MPa (10000Atm.)
no DOI — not checked10.1016/j.supflu.2015.02.010_bib0355
no DOI — not checkedThe extraction quench technique for determination of the thermodynamic properties of solute complexes: application to quartz solubility in fluid mixtures
no DOI — not checkedThermodynamic model for mineral solubility in aqueous fluids: theory, calibration and application to model fluid-flow systems
no DOI — not checkedRevised quartz solubility temperature dependence equation along the water–vapor saturation curve
no DOI — not checked10.1016/j.supflu.2015.02.010_bib0460
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