An equation of state for silicate melts.: II.: Calibration of volumetric properties at 105 Pa

被引:49
作者
Ghiorso, MS
Kress, VC
机构
[1] Univ Chicago, Dept Geophys Sci, Chicago, IL 60637 USA
[2] Univ Washington, Dept Earth & Space Sci, Seattle, WA 98195 USA
关键词
D O I
10.2475/ajs.304.8-9.679
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Reference pressure (10(5) Pa) parameters for the silicate liquid equation of state of Ghiorso (2004a) are calibrated from literature data on measurements of densities and sound speeds. A model for the temperature- and compositionally-dependent, reference-pressure volume (density) in the system K2O-Na2O-CaO-MgO-FeO-NiO-CoO-Fe2O3-Al2O3-TiO2-SiO2 is obtained. Precision of data recovery is 0.76 percent (one root-mean-square residual). Linear mixing relations for model parameters are utilized in this calibration with the inclusion of quadratic terms between soda and titania and potash and titania to account for the effect of alkali metals on the partial molar volume of TiO2. Liquids in the system CaO-Al2O3-SiO2 with molar ratios of CaO/SiO2 < 0.5 are excluded from this analysis in order to avoid the inclusion of additional non-linear terms. Iron-bearing systems are modeled by first "speciating" the liquid to obtain molecular proportions of FeO, FeO1.5 (Fe2O3) and FeO1.3 (Fe0.42+Fe0.63+O1.3). Partial molar properties are extracted for all three iron oxides. This procedure is followed because (1) it affords an internally consistent means of extrapolating previously calibrated models of iron-redox equilibria in silicate melts to elevated pressure, and (2) it results in significant improvements in model recovery of density measurements on Fe-bearing systems. The model partial molar volume of FeO1.3 is similar to12 percent smaller than a linear combination of the fully oxidized and reduced endmembers. Internally consistent expressions for the reference pressure compressibility and its temperature dependence are formulated from a calibration of sound speeds in molten liquids. A model for the temperature- and compositionally-dependent sound speed in the system K2O-Na2O-CaO-MgO-FeO-Fe2O3-Al2O3-TiO2-SiO2, is obtained. Precision of data recovery is 1.7 percent. Mixing relations identical to the volume model are adopted for consistency with the inclusion of an additional quadratic composition term in soda and alumina.
引用
收藏
页码:679 / 751
页数:73
相关论文
共 50 条
[1]  
BAIDOV VV, 1968, SOV PHYS DOKL, V1, P64
[2]  
Bevington R., 1969, DATA REDUCTION ERROR
[3]   The compressibilities of certain molten alkali silicates and borates [J].
Bockris, J. O'M. ;
Kojonen, E. .
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1960, 82 (17) :4493-4497
[4]  
BOCKRIS JO, 1955, FARADAY SOC T, V52, P299
[5]   DENSITY CALCULATIONS FOR SILICATE LIQUIDS .1. REVISED METHOD FOR ALUMINOSILICATE COMPOSITIONS [J].
BOTTINGA, Y ;
WEILL, D ;
RICHET, P .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1982, 46 (06) :909-919
[6]   DENSITY CALCULATIONS FOR SILICATE LIQUIDS - REPLY [J].
BOTTINGA, Y ;
WEILL, DF ;
RICHET, P .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1984, 48 (02) :409-414
[7]   DENSITIES OF LIQUID SILICATE SYSTEMS CALCULATED FROM PARTIAL MOLAR VOLUMES OF OXIDE COMPONENTS [J].
BOTTINGA, Y ;
WEILL, DF .
AMERICAN JOURNAL OF SCIENCE, 1970, 269 (02) :169-&
[8]   NONLINEAR COMPOSITION DEPENDENCE OF MOLAR VOLUME OF MELTS IN THE CAO-AL2O3-SIO2 SYSTEM [J].
COURTIAL, P ;
DINGWELL, DB .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1995, 59 (18) :3685-3695
[9]   High-temperature densities of some mantle melts [J].
Courtial, P ;
Ohtani, E ;
Dingwell, DB .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1997, 61 (15) :3111-3119
[10]  
Courtial P, 1999, AM MINERAL, V84, P465