Reference health
The influence of the alkaline earth cations, magnesium, calcium, and barium on the dissolution kinetics of quartz
00217-2/badge.svg){kind=icon}
37/37 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.
11 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 37 checked references that resolve
resolves10.1139/v60-138
THEORETICAL STUDIES ON SOLVATION: PART II. NEW THEORY FOR EVALUATION OF IONIC SOLVATION NUMBER FOR DIVALENT IONS AT 25 °C
resolves10.4319/lo.1994.39.1.0099
Experimental dissolution of diatom silica in concentrated salt solutions and implications for paleoenvironmental reconstruction
resolves10.1016/0016-7037(88)90222-0
The dissolution of quartz in dilute aqueous solutions of organic acids at 25°C
resolves10.1016/0016-7037(94)90487-1
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
resolves10.1002/zaac.19593010516
Über die Hydroxylgruppen an der Oberfläche des Amorphen Siliciumdioxyds „Aerosil”︁ und ihre Reaktionen
resolves10.1038/355157a0
Control of dissolution rates of orthosilicate minerals by divalent metal–oxygen bonds
resolves10.1016/0016-7037(90)90291-R
Mechanisms of silica dissolution as inferred from the kinetic isotope effect
resolves10.2475/ajs.277.1.38
Influence of seed crystals on the precipitation of calcite and aragonite
resolves10.2475/ajs.294.6.665
The dissolution kinetics of quartz in sodium chloride solutions at 25 degrees to 300 degrees C
resolves10.1029/95JB02155
Geochemical controls on the kinetics of quartz fracture at subcritical tensile stresses
resolves10.1016/0016-7037(90)90431-J
Kinetics of quartz dissolution in electrolyte solutions using a hydrothermal mixed flow reactor
resolves10.1016/0016-7037(95)00116-6
Crystal chemical controls on the dissolution kinetics of the isostructural sulfates: Celestite, anglesite, and barite
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
resolves10.1021/j100786a007
The Exchange of Twenty Metal Ions with the Weakly Acidic Silanol Group of Silica Gel<sup>1,2</sup>
resolves10.1016/0016-7037(83)90279-X
A method of calculating quartz solubilities in aqueous sodium chloride solutions
resolves10.1016/0016-7037(82)90135-1
An equation correlating the solubility of quartz in water from 25° to 900°C at pressures up to 10,000 bars
resolves10.1016/0016-7037(86)90243-7
The coordination chemistry of weathering: I. Dissolution kinetics of δ-Al2O3 and BeO
resolves10.1016/0016-7037(90)90109-X
Dissolution of quartz in aqueous basic solution, 106–236°C: Surface kinetics of “perfect” crystallographic faces
resolves10.1006/jcis.1994.1117
The Role of Surface Complexation in the Dissolution Kinetics of Silica: Effects of Monovalent and Divalent Ions at 25°C
resolves10.1039/FT9928802021
Dissolution kinetics of silica between 5 and 35 °C. Application of a titrimetric method
resolves10.1016/0021-9797(75)90065-X
Coagulation of colloidal silica by calcium ions, mechanism, and effect of particle size
resolves10.1016/0021-9797(73)90386-X
Effect of adsorbed alumina on the solubility of amorphous silica in water
resolves10.2475/ajs.290.3.263
Ab-initio quantum mechanical calculations of water-rock interactions; adsorption and hydrolysis reactions
resolves10.1016/0021-9797(66)90039-7
The role of hydration in the adsorption of alkaline earth ions onto quarts
resolves10.1524/zpch.1973.85.1-4.038
An NMR Study of Water Adsorbed on Silica. The Influence of Cations Exchanged on the Surface. III
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
resolves10.1016/S0022-0728(69)80140-3
The electrical double layer on silica in the presence of bivalent counter-ions
resolves10.1016/0021-9797(79)90307-2
The initial kinetics of the dissolution of vitreous silica in aqueous media
The 11 references without a DOI — listed, not checked
no DOI — not checked10.1016/S0016-7037(97)00217-2_bib8
no DOI — not checked10.1016/S0016-7037(97)00217-2_bib11
no DOI — not checkedKinetic and Thermodynamic Controls on Silica Reactivity in Weathering Environments
no DOI — not checkedSilica-water interactions
no DOI — not checkedThe sedimentary genesis of hydrothermal fluids
no DOI — not checked10.1016/S0016-7037(97)00217-2_bib30
no DOI — not checked10.1016/S0016-7037(97)00217-2_bib33
no DOI — not checkedThe role of salts in the dissolution of powdered quartz
no DOI — not checkedTransition state theory
no DOI — not checkedAtomic treatment of mineral-water surface reactions
no DOI — not checkedDetermination of reactive silicate
What this badge says. CiteStamped means the CHECKABLE references of this
work were clean at the dated check: each resolved to a known work in a public registry, and none
carried a retraction notice at that time. It says nothing about the quality, findings,
or importance of the work itself, and nothing about references deposited without a DOI.
checked 2026-07-22 — re-checked daily as this page is visited; titles and statuses come from Crossref and DataCite and are not part of the signed record
Embed this badge
Both snippets point at the live badge image and link back to this page. The badge re-renders from the daily check, so an embed never goes stale by more than a day of visits.
<a href="https://citestamp.com/citestamped/10.1016/s0016-7037(97)00217-2"><img src="https://citestamp.com/citestamped/10.1016/s0016-7037(97)00217-2/badge.svg" alt="CiteStamped reference-health badge" width="460" height="64"></a>
[00217-2/badge.svg)](https://citestamp.com/citestamped/10.1016/s0016-7037(97)00217-2)