Mapping the thermal structure of solid-media pressure assemblies

被引:124
作者
Watson, EB [1 ]
Wark, DA
Price, JD
Van Orman, JA
机构
[1] Rensselaer Polytech Inst, Dept Earth & Environm Sci, Troy, NY 12180 USA
[2] Carnegie Inst Washington, Geophys Lab, DTM, Washington, DC 20015 USA
基金
美国国家科学基金会;
关键词
D O I
10.1007/s00410-001-0327-4
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 refractory oxides MgO and Al2O3 are the most commonly used insulator, filler materials in solid-media pressure assemblies. These oxides react with one another at high temperatures and pressures, forming a well-defined layer of spinel (similar toMgAl(2)O(4)) at the contact. The spinel layer widens in proportion to the square root of time at a rate that also depends systematically upon temperature and pressure. On the basis of 44 piston-cylinder runs spanning 1.200-2,000 degreesC and 1.0-4.0 GPa. we present a general relationship describing the width (AY) of the spinel layer as a function of time (t. in s). temperature (T. in K) and pressure (R in GPa): DeltaX = [8.58 x 10(11) (.) exp(-48865/T - 2.08 (.) p(1/2))(.) t] (1/2). If the pressure and duration of an experiment are known (as is usually the case) this calibration makes it possible to calculate the temperature to within a few degrees at any location in a solid-media assembly where MgO and Al2O3 are in contact (at T above similar to1,200 degreesC - simply by measuring the width of the spinel layer with an optical microscope. Application of this "reaction-progress" thermometer to the 13- and 19-mm diameter piston-cylinder assemblies used in the RPI lab confirms generally parabolic axial T gradients with acceptably broad hot spots. Three-dimensional maps of the 19-mm assembly reveal a radial component to the thermal field. with somewhat higher temperatures near the graphite heating element (i.e., a saddle-shaped hot region). Two exploratory experiments in a multi-anvil apparatus at 14 GPa (1,700 and 1,975 degreesC) confirm that the reaction-progress technique will work at pressures well above 4 GPa. The piston-cylinder-based calibration predicts DeltaX to within a factor of two in the two multi-anvil runs, and relative changes in T along the assembly can be readily mapped. However, additional high-pressure calibration points will be needed before the thermometer can be used in quantitative multi-anvil applications. The spinel reaction-progress thermometer is easily implemented, and should allow other researchers to map the thermal structures of their own assemblies in a single experiment with one thermocouple.
引用
收藏
页码:640 / 652
页数:13
相关论文
共 26 条
[1]   High pressure transitions in the system MgAl2O4-CaAl2O4:: a new hexagonal aluminous phase with implication for the lower mantle [J].
Akaogi, M ;
Hamada, Y ;
Suzuki, T ;
Kobayashi, M ;
Okada, M .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1999, 115 (01) :67-77
[2]   Mineralogy of the Martian interior up to core-mantle boundary pressures [J].
Bertka, CM ;
Fei, YW .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1997, 102 (B3) :5251-5264
[3]   APPARATUS FOR PHASE-EQUILIBRIUM MEASUREMENTS AT PRESSURES UP TO 50-KILOBARS AND TEMPERATURES UP TO 1750-DEGREES-C [J].
BOYD, FR ;
ENGLAND, JL .
JOURNAL OF GEOPHYSICAL RESEARCH, 1960, 65 (02) :741-748
[5]   CHANGES IN VISCOSITY AND STRUCTURE OF MELT OF NAALSI2O6 COMPOSITION AT HIGH-PRESSURES [J].
KUSHIRO, I .
JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (35) :6347-6350
[6]   CUMULATE MATURATION AND MELT MIGRATION IN A TEMPERATURE-GRADIENT [J].
LESHER, CE ;
WALKER, D .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1988, 93 (B9) :10295-10311
[7]   SOLUTION PROPERTIES OF SILICATE LIQUIDS FROM THERMAL-DIFFUSION EXPERIMENTS [J].
LESHER, CE ;
WALKER, D .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1986, 50 (07) :1397-1411
[8]   A HIGH-RESOLUTION ELECTRON-MICROSCOPY STUDY OF MGO/AL2O3 INTERFACES AND MGAL2O4 SPINEL FORMATION [J].
LI, DX ;
PIROUZ, P ;
HEUER, AH ;
YADAVALLI, S ;
FLYNN, CP .
PHILOSOPHICAL MAGAZINE A-PHYSICS OF CONDENSED MATTER STRUCTURE DEFECTS AND MECHANICAL PROPERTIES, 1992, 65 (02) :403-425
[9]  
LIDE DR, 1998, HDB CHEM PHYSICS
[10]  
MACKENZIE KJD, 1981, J MATER SCI, V16, P579, DOI 10.1007/BF02402773