Experimental study of kyanite dissolution rates as a function of chemical affinity and solution composition

[1]  J. Dandurand,et al.  An experimental study of kaolinite dissolution and precipitation kinetics as a function of chemical affinity and solution composition at 150°C, 40 bars, and pH 2, 6.8, and 7.8 , 1997 .

[2]  S. Gíslason,et al.  Kinetic and thermodynamic properties of moganite, a novel silica polymorph , 1997 .

[3]  R. Pabalan,et al.  Reaction kinetics and thermodynamics of aqueous dissolution and growth of analcime and Na-clinoptilolite at 25 degrees C , 1996 .

[4]  A. Lasaga.  Chapter 2. FUNDAMENTAL APPROACHES IN DESCRIBING MINERAL DISSOLUTION AND PRECIPITATION RATES , 1995 .

[5]  E. Oelkers,et al.  Experimental study of anorthite dissolution and the relative mechanism of feldspar hydrolysis , 1995 .

[6]  H. Helgeson,et al.  Thermodynamic Properties of Aqueous Species and the Solubilities of Minerals at High Pressures and Temperatures; the System Al 2 O 3 -H 2 O-NaCl , 1995, American Journal of Science.

[7]  E. Oelkers,et al.  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 , 1995 .

[8]  E. Oelkers,et al.  Dissolution and crystallization rates of silicate minerals as a function of chemical affinity , 1995 .

[9]  E. Oelkers,et al.  Experimental study of K-feldspar dissolution rates as a function of chemical affinity at 150°C and pH 9 , 1994 .

[10]  J. Tester,et al.  Correlating quartz dissolution kinetics in pure water from 25 to 625°C , 1994 .

[11]  Kathryn L. Nagy,et al.  Chemical weathering rate laws and global geochemical cycles , 1994 .

[12]  E. Oelkers,et al.  The effect of aluminum, pH, and chemical affinity on the rates of aluminosilicate dissolution reactions , 1994 .

[13]  M. Barton.  The Al2SiO5 polymorphs: Derrill M. Kerrick. reviews in mineralogy, volume 22, mineralogical society of America, 1991, xii + 406 p., US $20.00 (ISBN 0-939950-27-8) , 1994 .

[14]  Harald Sverdrup,et al.  Calculating field weathering rates using a mechanistic geochemical model PROFILE , 1993 .

[15]  A. Lasaga,et al.  Free energy dependence of albite dissolution kinetics at 80°C and pH 8.8 , 1993 .

[16]  T. J. Wolery,et al.  EQ3NR, a computer program for geochemical aqueous speciation-solubility calculations: Theoretical manual, user`s guide, and related documentation (Version 7.0); Part 3 , 1992 .

[17]  A. Lasaga,et al.  Dissolution and precipitation kinetics of gibbsite at 80°C and pH 3: The dependence on solution saturation state , 1992 .

[18]  E. Oelkers,et al.  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 , 1992 .

[19]  N. M. Rose.  Dissolution rates of prehnite, epidote, and albite , 1991 .

[20]  A. Lasaga,et al.  Dissolution and precipitation kinetics of kaolinite at 80 degrees C and pH 3; the dependence on solution saturation state , 1991 .

[21]  J. Drever,et al.  Aquatic Chemical Kinetics , 1991 .

[22]  P. Dove.  Reply to Comment on “Kinetics of quartz dissolution in electrolyte solutions using a hydrothermal mixed flow reactor” , 1990 .

[23]  D. Pattison.  P–T Conditions and the Influence of Graphite on Pelitic Phase Relations in the Ballachulish Aureole, Scotland , 1989 .

[24]  G. J. Woodsworth,et al.  Aluminum silicates in the Mount Raleigh pendant, British Columbia , 1989 .

[25]  K. Knauss,et al.  Muscovite dissolution kinetics as a function of pH and time at 70°C , 1989 .

[26]  B. Wehrli,et al.  The coordination chemistry of weathering: III. A generalization on the dissolution rates of minerals , 1988 .

[27]  H. Helgeson,et al.  Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions. III. Activated complexes and the pH-dependence of the rates of feldspar, pyroxene, wollastonite, and olivine hydrolysis , 1987 .

[28]  S. Bohlen.  Pressure-Temperature-Time Paths and a Tectonic Model for the Evolution of Granulites , 1987, The Journal of Geology.

[29]  J. A. Schramke,et al.  The reaction muscovite + quartz andalusite + K-feldspar + water; Part 1, Growth kinetics and mechanism , 1987 .

[30]  S. Wickham.  Crustal Anatexis and Granite Petrogenesis During Low-pressure Regional Metamorphism: The Trois Seigneurs Massif, Pyrenees, France , 1987 .

[31]  K. Knauss,et al.  Dependence of albite dissolution kinetics on ph and time at 25°c and 70°c , 1986 .

[32]  G. Furrer,et al.  The coordination chemistry of weathering: II. Dissolution of Fe(III) oxides , 1986 .

[33]  G. Furrer,et al.  The coordination chemistry of weathering: I. Dissolution kinetics of δ-Al2O3 and BeO , 1986 .

[34]  Lei Chou,et al.  Steady-state kinetics and dissolution mechanisms of albite , 1985 .

[35]  M. L. Williams,et al.  The Effects of Fe3³ and Mn3³ on Aluminum Silicate Phase Relations in North-Central New Mexico, U.S.A. , 1985 .

[36]  P. Aagaard,et al.  Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions. II. Rate constants, effective surface area, and the hydrolysis of feldspar , 1984 .

[37]  Lei Chou,et al.  Study of the weathering of albite at room temperature and pressure with a fluidized bed reactor , 1984 .

[38]  P. Aagaard,et al.  Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions; I, Theoretical considerations , 1982 .

[39]  J. D. Rimstidt,et al.  The kinetics of silica-water reactions , 1980 .

[40]  M. J. Holdaway.  Significance of chloritoid-bearing and staurolite-bearing rocks in the Picuris Range, New Mexico , 1978 .

[41]  P. Aagaard,et al.  Thermodynamic and kinetic constraints on the dissolution of feldspars , 1977 .

[42]  D. Kerrick.  Experimental determination of muscovite + quartz stability with P H2O total , 1972 .

[43]  M. J. Holdaway.  Stability of andalusite and the aluminum silicate phase diagram , 1971 .

[44]  W. S. MacKenzie,et al.  Some aspects of experimental petrology , 1969 .

[45]  W. Fyfe.  Some second thoughts on Al 2 O 3 -SiO 2 , 1969 .

[46]  B. W. Evans.  Application of a reaction-rate method to the breakdown equilibria of muscovite and muscovite plus quartz , 1965 .

[47]  L. Marini,et al.  Proceedings of the Rome Seminar on Environmental Geochemistry , 1998 .

[48]  Eric H. Oelkers,et al.  Physical and chemical properties of rocks and fluids for chemical mass transport calculations , 1996 .

[49]  P. Brady.  Physics and chemistry of mineral surfaces , 1996 .

[50]  A. Blum,et al.  Feldspar dissolution kinetics , 1995 .

[51]  H. Sverdrup,et al.  Estimating field weathering rates using laboratory kinetics , 1995 .

[52]  E. Oelkers.  Experimental Study of Kyanite Dissolution Rates as a Function of Al and Si Concentration , 1994 .

[53]  Jean-Luc Devidal.  Solubilité et cinétique de dissolution/précipitation de la kaolinite en milieu hydrothermal : approche expérimentale et modélisation , 1994 .

[54]  P. Sabatier,et al.  Experimental study of kyanite dissolution rates as a function of A1 and Si concentration , 1994 .

[55]  P. Dove,et al.  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 , 1994 .

[56]  E. Oelkers,et al.  The dissolution rate of albite as a function of chemical affinity and the stoichiometry of activated complexes in aluminosilicate dissolution reactions , 1992 .

[57]  D. Kerrick.  The Al[2]Sio[5] polymorphs , 1990 .

[58]  Patrick V. Brady,et al.  Kinetics of quartz dissolution at low temperatures , 1990 .

[59]  C. Steefel,et al.  Dissolution and Precipitation Kinetics of Kaolinite: Initial Results at 80°C with Application to Porosity Evolution in a Sandstone , 1990 .

[60]  K. Knauss,et al.  The dissolution kinetics of quartz as a function of pH and time at 70°C , 1988 .

[61]  A. Lasaga.  Transition state theory , 1981 .

[62]  G. Chinner.  The significance of the aluminium silicates in metamorphism , 1966 .

[63]  C. Burnham.  Refinement of the crystal structure of kyanite , 1963 .