Reference health
The dissolution kinetics of amorphous silica into sodium chloride solutions: effects of temperature and ionic strength
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30/30 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.
8 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 30 checked references that resolve
resolves10.1016/0016-7037(88)90222-0
The dissolution of quartz in dilute aqueous solutions of organic acids at 25°C
resolves10.2475/ajs.294.6.665
The dissolution kinetics of quartz in sodium chloride solutions at 25 degrees to 300 degrees C
resolves10.1016/S0016-7037(99)00218-5
The dissolution kinetics of quartz in aqueous mixed cation solutions
resolves10.1016/0016-7037(90)90431-J
Kinetics of quartz dissolution in electrolyte solutions using a hydrothermal mixed flow reactor
resolves10.1016/S0016-7037(97)00217-2
The influence of the alkaline earth cations, magnesium, calcium, and barium on the dissolution kinetics of quartz
resolves10.1016/0016-7037(83)90279-X
A method of calculating quartz solubilities in aqueous sodium chloride solutions
resolves10.1016/0016-7037(90)90109-X
Dissolution of quartz in aqueous basic solution, 106–236°C: Surface kinetics of “perfect” crystallographic faces
resolves10.1039/FT9928802021
Dissolution kinetics of silica between 5 and 35 °C. Application of a titrimetric method
resolves10.1039/FT9928800233
Investigation of the pH dependence of the kinetics of quartz dissolution at 25 °C
resolves10.1016/0021-9797(72)90174-9
Adsorption of hydrolyzable metal ions at the oxide—water interface. III. A thermodynamic model of adsorption
resolves10.1016/0016-7037(88)90055-5
The dissolution kinetics of quartz as a function of pH and time at 70°C
resolves10.1016/0022-3093(94)90100-7
Dissolution kinetics of silica glass as a function of pH between 40 and 85°C
resolves10.1016/0016-7037(94)00232-B
Precipitation and dissolution rate constants for cristobalite from 150 to 300°C
resolves10.1016/0016-7037(84)90274-6
Glass transitions and thermodynamic properties of amorphous SiO2, NaAlSinO2n+2 and KAlSi3O8
resolves10.1016/0016-7037(86)90033-5
Mineral/solution reaction rates in a mixed flow reactor: Wollastonite hydrolysis
resolves10.1038/364776a0
Physical surface-complexation models for sorption at the mineral–water interface
resolves10.1016/S0016-7037(97)00127-0
Solvation and electrostatic model for specific electrolyte adsorption
resolves10.1016/S0167-2738(97)00289-0
The kinetics of dissolution of silica ?Monospher? into water at different concentrations of background electrolyte
resolves10.1016/0016-7037(94)90020-5
Correlating quartz dissolution kinetics in pure water from 25 to 625°C
resolves10.1016/0021-9797(79)90307-2
The initial kinetics of the dissolution of vitreous silica in aqueous media
The 8 references without a DOI — listed, not checked
no DOI — not checked10.1016/S0016-7037(00)00487-7_BIB7
no DOI — not checkedLeaching of mineral and glass surfaces
no DOI — not checkedSilica–water interactions
no DOI — not checkedMolecules as models for bonding in silicates
no DOI — not checked10.1016/S0016-7037(00)00487-7_BIB22
no DOI — not checkedPolster W. (1994) Hydrothermal precipitation and dissolution of silica Part 1. Conditions in geothermal fields and sedimentary basins, Part 2. Experimental evaluation of kinetics. Ph.D. Dissertation, Penn State Univ.
no DOI — not checkedDetermination of reactive silica
no DOI — not checkedWeissbart E. J. (1997) The leached layer formed on wollastonite in an acid environment. M.S. Thesis, VA Polytech. Inst. State Univ.
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