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E. Stolper (1982)
The speciation of water in silicate meltsGeochimica et Cosmochimica Acta, 46
P. McMillan, S. Jakobsson, J. Holloway, L. Silver (1983)
A note on the Raman spectra of water-bearing albite glassesGeochimica et Cosmochimica Acta, 47
H. Shaw (1964)
Theoretical Solubility of H2O in Silicate Melts Quasi-Crystalline ModelsThe Journal of Geology, 72
BO Mysen, D Virgo, WJ Harrison, CM Scarfe (1980)
Solubility mechanisms of H2O in silicate melts at high temperatures and pressures: a Raman spectroscopic studyAm Mineral, 65
CW Burnham, NF Davis (1974)
The role of H2O in silicate melts. II. Thermodynamic and phase relations in the system NaAl-Si3O8-H2O to 10 kilobars and 1,000° CAm J Sci, 274
JR Holloway (1981)
Advances in physical geochemistry, vol 1
GP Orlova (1962)
The solubility of water in albite meltsInt Geol Rev, 6
G. Kennedy, G. Wasserburg, H. Heard, R. Newton (1962)
The upper three-phase region in the system SiO 2 -H 2 OAmerican Journal of Science, 260
C. Burnham, N. Davis (1974)
The role of H 2 O in silicate melts; II, Thermodynamic and phase relations in the system NaAlSi 3 O 8 -H 2 O to 10 kilobars, 700 degrees to 1100 degrees CAmerican Journal of Science, 274
Donald Dingwell, D. Harris, C. Scarfe (1984)
The Solubility of H2O in Melts in the System SiO2-Al2O3-Na2O-K2O at 1 to 2 KbarsThe Journal of Geology, 92
B. Mysen (1977)
The solubility of H2O and CO2 under predicted magma genesis conditions and some petrological and geophysical implicationsReviews of Geophysics, 15
D. Hamilton, C. Burnham, E. Osborn (1964)
The Solubility of Water and Effects of Oxygen Fugacity and Water Content on Crystallization in Mafic MagmasJournal of Petrology, 5
S Oxtoby, DL Hamilton (1978)
Progress in experimental petrology. Fourth progress report of research supported by NERC
F. Freund, B. Mysen, D. Virgo (1980)
Solubility mechanisms of H 2 O in silicate melts at high pressures and temperatures; a Raman spectroscopic study; discussion and replyAmerican Mineralogist, 67
C. Burnham (1981)
The nature of multicomponent aluminosilicate meltsPhysics and Chemistry of The Earth
CW Burnham, NF Davis (1971)
The role of H2O in silicate melts. I. P-V-T relations in the system NaAlSi3O8-H2O to 10 kilobars at 1,000° CAm J Sci, 270
G. Orlova (1964)
SOLUBILITY OF WATER IN ALBITE MELTS -UNDER PRESSUREInternational Geology Review, 6
HS Yoder (1965)
Diopside-anorthite-water at five and ten kilobars and its bearing on explosive volcanismCarnegie Institute Washington Yearb. K, 64
RW Goranson (1937)
The osmotic pressure of silicate meltsAm Mineral, 22
S. Oxtoby, D. Hamilton (1978)
The discrete association of water with Na2O and SiO2 in NaAl silicate meltsContributions to Mineralogy and Petrology, 66
C. Burnham, John Holloway, N. Davis (1969)
Thermodynamic properties of water to 1,000 C and 10,000 bars
E. Stolper (1982)
Water in silicate glasses: An infrared spectroscopic studyContributions to Mineralogy and Petrology, 81
C. Burnham, R. Jahns (1962)
A method for determining the solubility of water in silicate meltsAmerican Journal of Science, 260
R. Goranson (1937)
Silicate-water systems: the “osmotic pressure” of silicate meltsAmerican Mineralogist, 22
C. Burnham, N. Davis (1971)
The role of H 2 O in silicate melts; I, P-V-T relations in the system NaAlSi 3 O 8 -H 2 O to 10 kilobars and 1000 degrees CAmerican Journal of Science, 270
G. Wasserburg (1957)
The Effects of H2O in Silicate SystemsThe Journal of Geology, 65
C. Burnham (1975)
Water and magmas; a mixing modelGeochimica et Cosmochimica Acta, 39
G. Walrafen (1964)
Raman Spectral Studies of Water StructureJournal of Chemical Physics, 40
P. McMillan, R. Remmele (1986)
Hydroxyl sites in SiO2 glass: a note on infrared and Raman spectraAmerican Mineralogist, 71
DE Voigt, RJ Bodnar, JG Blencoe (1981)
Water solubility in melts of alkali feldspar composition at 5 kbar, 950° CTrans Am Geophys Union, 62
DB Stewart (1967)
Four-phase curve in the system CaAl2Si2O8- SiO2-H2O between 1 and 10 kilobarsSchweiz Mineral Petrogr Mitt, 47
We have measured the water solubility between 1 atmosphere and 5 kilobars for a calcium aluminosilicate melt of molar composition CaO 0.28, Al2O3 0.06, SiO2 0.66 (An9Wo38Qz53). The water contents were measured via thermogravimetric analysis of isobarically quenched glasses, and range from 0.121 wt% H2O near 1 aim to 9.25 wt% H2O at 5 kilobars. The molar water solubility lies between those of SiO2 and albite melts below around three kilobars, and crosses the albite solubility curve above this pressure. The present results are compared with data in the literature on related calcium aluminosilicate melts. There seems to be little variation of water solubility with composition for calcium aluminosilicate melts, unlike analogous alkali aluminosilicate compositions. Examination of the data suggests that there may be a maximum in molar water solubility along the albite-anorthite join.
Contributions to Mineralogy and Petrology – Springer Journals
Published: Oct 22, 2004
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