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THERMODYNAMIC MODEL FOR DIFFUSION CONTROLLED REACTION RIM GROWTH IN A BINARY SYSTEM: APPLICATION TO THE FORSTERITE-ENSTATITE-QUARTZ SYSTEM
被引:30
|作者:
Abart, R.
[1
]
Petrishcheva, E.
[1
]
Fischer, F. D.
[2
]
Svoboda, J.
[3
]
机构:
[1] Free Univ Berlin, Inst Geol Sci, D-12249 Berlin, Germany
[2] Univ Leoben, Inst Mech, A-8700 Leoben, Austria
[3] Acad Sci Czech Republic, Inst Phys Mat, CZ-61662 Brno, Czech Republic
关键词:
GRAIN-BOUNDARY DIFFUSION;
SELF-DIFFUSION;
KINETICS;
PRINCIPLE;
EVOLUTION;
PHASES;
MG;
D O I:
10.2475/02.2009.02
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
We present a thermodynamic model for diffusion controlled growth of a reaction rim of phase gamma between the phases alpha and beta in a two component system. We investigate the case, where the reactant phase alpha has planar, cylindrical and spherical geometry and is embedded in a matrix of phase beta. We find that for non planar geometry and for the general case, where the molar volumes of the reactant phases are different, the rim growth rate depends on the matrix-inclusion arrangement. The model is applied to growth of enstatite reaction rims that form at quartz-forsterite interfaces. Two different geometrical setups are considered, namely a spherical grain of forsterite in a quartz matrix and a spherical quartz grain in a forsterite matrix. The enstatite rims are polycrystalline and transfer of the MgO and SiO(2) components across the growing rim occurs by a combination of volume- and grain boundary diffusion. For enstatite rims that were grown at experimental conditions of 1000 degrees C and 1 GPa (Milke and others, 2008) bulk mass transfer may be described by effective diffusion coefficients in the range of 1.8 (.) 10(-17) m(2)s(-1) <= D(SiO2) <= 1.1 (.) 10(-16)m(2)s-1 and 2.7 (.) 10(-17)m(2)s(-1) <= D(MgO) <= 1.6 (.) 10(-16) m(2)s(-1).
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页码:114 / 131
页数:18
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