Reference health
Coupled alkali-feldspar dissolution and secondary mineral precipitation in batch systems: 1. New experiments at 200 °C and 300 bars
66/66 checkable references clean · checked 2026-07-23
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 66 checked references that resolve
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Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions; I, Theoretical considerations
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Change in the dissolution rates of alkali feldspars as a result of secondary mineral precipitation and approach to equilibrium
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The use of a surface complexation model to describe the kinetics of ligand-promoted dissolution of anorthite
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Some factors affecting the dissolution kinetics of anorthite at 25°C
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Kinetic constraints on illitization reactions and the effects of organic diagenesis in sandstone/shale sequences
resolves10.1180/minmag.1989.053.372.02
The effect of organic acids on the dissolution of K-feldspar under conditions relevant to burial diagenesis
resolves10.1016/B0-08-043751-6/05075-1
Reaction Kinetics of Primary Rock-forming Minerals under Ambient Conditions
resolves10.1016/0009-2541(93)90123-Z
Free energy dependence of albite dissolution kinetics at 80°C and pH 8.8
resolves10.1016/0016-7037(76)90192-7
The dissolution kinetics of feldspars at 25°C and 1 atm CO2 partial pressure
resolves10.1016/0016-7037(88)90147-0
Surface chemistry of labradorite feldspar reacted with aqueous solutions at pH = 2, 3, and 12
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Leaching and reconstruction at the surfaces of dissolving chain-silicate minerals
resolves10.1016/0016-7037(90)90115-2
The hydrothermal transformation rate of kaolinite to muscovite/illite
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Kaolinized, potassium-leached zones at the contacts of the Garn Formation, Haltenbanken, mid-Norwegian continental shelf
resolves10.1180/claymin.1993.028.3.01
Depth-Dependent Transformation of Kaolinite to Dickite In Sandstones of the Norwegian Continental Shelf
resolves10.1016/0016-7037(94)90190-2
Experimental study of K-feldspar dissolution rates as a function of chemical affinity at 150°C and pH 9
resolves10.1016/S0016-7037(97)00122-1
The surface chemistry and structure of acid-leached albite: New insights on the dissolution mechanism of the alkali feldspars
resolves10.1016/0016-7037(68)90100-2
Evaluation of irreversible reactions in geochemical processes involving minerals and aqueous solutions—I. Thermodynamic relations
resolves10.1016/0016-7037(72)90022-1
Kinetics of mass transfer among silicates and aqueous solutions: Correction and clarification
resolves10.1016/0016-7037(69)90127-6
Evaluation of irreversible reactions in geochemical processes involving minerals and aqueous solutions—II. Applications
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Calculation of mass transfer in geochemical processes involving aqueous solutions
resolves10.1016/0016-7037(84)90294-1
Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions. II. Rate constants, effective surface area, and the hydrolysis of feldspar
resolves10.1016/0016-7037(94)90491-X
The albite-water system: Part I. The kinetics of dissolution as a function of pH at 100, 200 and 300°C
resolves10.1016/0016-7037(95)00075-B
The albite-water system: Part II. The time-evolution of the stoichiometry of dissolution as a function of pH at 100, 200, and 300°C
resolves10.1016/j.gca.2005.10.007
Dissolution kinetics as a function of the Gibbs free energy of reaction: An experimental study based on albite feldspar
resolves10.1016/0016-7037(90)90152-B
The formation of leached layers on albite surfaces during dissolution under hydrothermal conditions
resolves10.1007/s00269-003-0308-4
An EFTEM/HRTEM high-resolution study of the near surface of labradorite feldspar altered at acid pH: evidence for interfacial dissolution-reprecipitation
resolves10.1007/BF00974100
Electrical conductivity measurements of aqueous sodium chloride solutions to 600�C and 300 MPa
resolves10.1023/A:1005146332605
Conductivity of Dilute Aqueous Electrolyte Solutions at High Temperatures and Pressures Using a Flow Cell
resolves10.1021/jp0029818
Conductivity Measurements of Dilute Aqueous HCl Solutions to High Temperatures and Pressures Using a Flow-Through Cell
resolves10.2475/ajs.285.10.994
pH dependent changes in the rates and stoichiometry of dissolution of an alkali feldspar at room temperature
resolves10.1016/0016-7037(87)90284-5
Reaction rate-surface area relationships during the early stages of weathering. II. Data on eight additional feldspars
resolves10.1111/j.1525-1314.1998.00140.x
An internally consistent thermodynamic data set for phases of petrological interest
resolves10.1180/claymin.1986.021.4.10
The effect of fluid/rock ratio on feldspar dissolution and illite formation under reservoir conditions
resolves10.1016/0016-7037(91)90342-3
Characterization of laboratory weathered labradorite surfaces using X-ray photoelectron spectroscopy and transmission electron microscopy
resolves10.1016/0098-3004(92)90029-Q
SUPCRT92: A software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from 1 to 5000 bar and 0 to 1000°C
resolves10.1016/0016-7037(86)90031-1
Dependence of albite dissolution kinetics on ph and time at 25°c and 70°c
resolves10.2138/am-2004-11-1229
Coupled cation and oxygen-isotope exchange between alkali feldspar and aqueous chloride solution
resolves10.1016/0016-7037(76)90173-3
New data on the kinetics of the dissolution of alkali feldspars at 200°C in CO2 charged water
resolves10.1016/0016-7037(95)00255-X
Microtextural controls of weathering of perthitic alkali feldspars
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
resolves10.1038/334336a0
SIMS depth profiles of weathered plagioclase and processes affecting dissolved Al and Si in some acidic soil solutions
resolves10.1016/S0016-7037(00)00530-5
Early development of Al, Ca, and Na compositional gradients in labradorite leached in pH 2 HCl solutions
resolves10.1086/629504
Congruent and Incongruent Dissolution of Labradorite in Dilute, Acidic, Salt Solutions
resolves10.1016/0016-7037(94)90281-X
The effect of aluminum, pH, and chemical affinity on the rates of aluminosilicate dissolution reactions
resolves10.1130/0091-7613(2001)029<0843:IOCOSG>2.0.CO;2
Iron oxide coatings on sand grains from the Atlantic coastal plain: High-resolution transmission electron microscopy characterization
resolves10.1016/0016-7037(76)90090-9
Rate control in feldspar dissolution—II. The protective effect of precipitates
resolves10.1016/0016-7037(88)90181-0
Calculation of the thermodynamic and transport properties of aqueous species at high pressures and temperatures: Correlation algorithms for ionic species and equation of state predictions to 5 kb and 1000°C
resolves10.1016/S0016-7037(96)00339-0
Inorganic species in geologic fluids: Correlations among standard molal thermodynamic properties of aqueous ions and hydroxide complexes
resolves10.1016/0016-7037(90)90003-4
A new kinetic approach to modeling water-rock interaction: The role of nucleation, precursors, and Ostwald ripening
resolves10.1016/0016-7037(95)00057-7
Feldspar dissolution at 25°C and pH 3: Reaction stoichiometry and the effect of cations
resolves10.1016/S0016-7037(97)00009-4
Prediction of the thermodynamic properties of aqueous metal complexes to 1000°C and 5 kb
resolves10.1016/0016-7037(92)90292-Q
Surface reactions during the early stages of weathering of albite
resolves10.1016/j.gca.2006.07.013
Naturally weathered feldspar surfaces in the Navajo Sandstone aquifer, Black Mesa, Arizona: Electron microscopic characterization
The 18 references without a DOI — listed, not checked
no DOI — not checkedRates of congruent dissolution of feldspars in acid and alkaline hydrothermal solutions
no DOI — not checkedClay minerals in North Sea sandstones
no DOI — not checkedDislocation etch pits in quartz
no DOI — not checkedChemical interaction of feldspar and aqueous solutions
no DOI — not checkedMass transfer among minerals and hydrothermal solutions
no DOI — not checkedChemical alteration of feldspar: a comparative study using SIMS and HRTEM/EFTEM
no DOI — not checkedTransition state theory
no DOI — not checked10.1016/j.chemgeo.2008.09.014_bib53
no DOI — not checkedThe decomposition of microcline, albite, and nepheline in hot water
no DOI — not checkedDissolution and precipitation kinetics of sheet silicates
no DOI — not checkedMechanisms and rate laws in electrolyte crystal growth from aqueous solution
no DOI — not checkedThe oxygen isotope and cation exchange chemistry of feldspars
no DOI — not checkedReaction of microcline–perthite with aqueous solutions at 150 and 250 °C
no DOI — not checkedRocking autoclaves for hydrothermal experiments II: the flexible reaction cell system
no DOI — not checkedKinetics and modeling of alkali-feldspar dissolution in a hydrothermal acid solution
no DOI — not checked10.1016/j.chemgeo.2008.09.014_bib80
no DOI — not checkedFeldspar dissolution rates and clay precipitation in the Navajo aquifer at Black Mesa, Arizona, USA
no DOI — not checkedA new hypothesis for the slow feldspar dissolution in groundwater aquifers
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