NONLINEAR TEMPERATURE-DEPENDENCE OF LIQUID VOLUMES IN THE SYSTEM ALBITE-ANORTHITE-DIOPSIDE

被引:39
作者
KNOCHE, R
DINGWELL, DB
WEBB, SL
机构
[1] Bayerisches Geoinstitut, Universität Bayreuth, Bayreuth, W-8580
关键词
D O I
10.1007/BF00296578
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The temperature-dependent thermal expansivities of glasses and liquids in the ternary albite-anorthite-diopside have been determined using a combination of calorimetry, dilatometry and Pt and Ir double bob Archimedean densitometry. Supercooled liquid volumes and molar thermal expansivities were determined across the glass transition using a combination of scanning calorimetry and dilatometry, based upon the equivalence of relaxation of volume and enthalpy in the vicinity of the glass transition. Superliquidus volumes were determined using double Pt bob Archimedean densitometry at temperatures up to 1,650-degrees-C and double Ir bob densitometry at 1,800-degrees-C. Experimental access to liquid volumes near the glass transition temperatures (680-920-degrees-C) and at superliquidus temperatures (1,400-1,800-degrees-C) for these compositions results in the observation of a non-linear temperature dependence of molar volume, i.e., temperature-dependent thermal expansivities. The diopside composition exhibits the largest temperature dependence of thermal expansivity, decreasing by approximately 50% between 800 and 1,500-degrees-C. Linear extrapolation of the high-temperature volume data of diopside to 810-degrees-C would result in a 3% overestimation of the molar volume. The temperature dependence of the molar volume of anorthite is approximately linear. The thermal expansivities of the liquids in the albite-anorthite-diopside system appear to converge at high temperature. This study uses a combination of methods that allows interpolation rather than extrapolation of the extant melt-volume data into the petrologically meaningful (subliquidus) temperature range.
引用
收藏
页码:61 / 73
页数:13
相关论文
共 46 条
[1]   THERMAL-EXPANSION AND GLASS TRANSITION TEMPERATURES OF SYNTHETIC GLASSES OF PLAGIOCLASE-LIKE COMPOSITIONS [J].
ARNDT, J ;
HABERLE, F .
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1973, 39 (02) :175-183
[2]  
BERMAN H, 1942, HDB PHYSICAL CONSTAN, V36, P7
[3]   CALCULATION OF THE DENSITY AND THERMAL-EXPANSION COEFFICIENT OF SILICATE LIQUIDS [J].
BOTTINGA, Y ;
RICHET, P ;
WEILL, DF .
BULLETIN DE MINERALOGIE, 1983, 106 (1-2) :129-138
[4]   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-&
[5]  
Bowen NL, 1915, AM J SCI, V40, P161
[6]   VISCOSITY OF LIQUID ANORTHITE [J].
CUKIERMAN, M ;
UHLMANN, DR .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (23) :4920-4923
[7]   PROPERTIES OF SODA ALUMINOSILICATE GLASSES .1. REFRACTIVE INDEX, DENSITY, MOLAR REFRACTIVITY, AND INFRARED ABSORPTION SPECTRA [J].
DAY, DE ;
RINDONE, GE .
JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1962, 45 (10) :489-496
[8]   MELT DENSITIES IN THE NA2O-FEO-FE2O3-SIO2 SYSTEM AND THE PARTIAL MOLAR VOLUME OF TETRAHEDRALLY-COORDINATED FERRIC IRON IN SILICATE MELTS [J].
DINGWELL, DB ;
BREARLEY, M ;
DICKINSON, JE .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1988, 52 (10) :2467-2475
[9]  
DINGWELL DB, 1989, PHYS CHEM MINER, V16, P508
[10]   EFFECTS OF STRUCTURAL RELAXATION ON CATIONIC TRACER DIFFUSION IN SILICATE MELTS [J].
DINGWELL, DB .
CHEMICAL GEOLOGY, 1990, 82 (3-4) :209-216