Atomistic simulation of the mechanisms of noble gas incorporation in minerals

被引:21
作者
Du, Z. [1 ,2 ,3 ]
Allan, N. L. [1 ]
Blundy, J. D. [2 ]
Purton, J. A. [4 ]
Brooker, R. A. [5 ]
机构
[1] Univ Bristol, Sch Chem, Bristol BS8 1TS, Avon, England
[2] Univ Bristol, Dept Earth Sci, CETSEI, Bristol BS8 1RJ, Avon, England
[3] UCL, Dept Chem, London WC1H 0AJ, England
[4] CLRC, Daresbury Lab, Warrington WA4 4AD, Cheshire, England
[5] UCL, Dept Earth Sci, London WC1E 6BT, England
关键词
D O I
10.1016/j.gca.2007.10.007
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
Atomistic simulations have been carried out to investigate the mechanisms of noble gas incorporation in minerals using both the traditional two-region approach and the "supercell" method. The traditional two-region approach has been used to calculate defect energies for Ne, Ar, Kr and Xe incorporation in MgO, CaO, diopside and forsterite in the static limit and at one atmosphere pressure. The possibilities of noble gas incorporation via both substitution and interstitial mechanisms are studied. The favored mechanism varies from mineral to mineral and from noble gas to noble gas. In all minerals studied, the variation of the solution energies of noble gas substitution with atomic radius appears approximately parabolic, analogous to those for 1(+), 2(+), 3(+) and 4(+) trace element incorporation on crystal lattice sites. Noble gas solution energies thus also fall on a curve, similar to those previously observed for cations with different charges, but with much lower curvature. The "supercell" method has been used to investigate the pressure dependence of noble gas incorporation in the same systems. Results indicate a large variation of the solubility of the larger noble gases, Kr and Xe with pressure. In addition, explicit simulation of incorporation at the (001) surface of MgO shows that the solubility of the heavier noble gases may be considerably enhanced by the presence of interfaces. (C) 2007 Elsevier Ltd. All rights reserved.
引用
收藏
页码:554 / 573
页数:20
相关论文
共 64 条
[1]  
ALLAN, 1987, J CHEM SOC F2, V83, P1675
[2]  
ALLAN NL, 1993, ADV SOLID STATE CHEM, V3, P221
[3]  
ALLAN NL, 1987, ADV CERAM, V23, P257
[4]  
ALLEGRE CJ, 1987, EARTH PLANET SC LETT, V81, P127, DOI 10.1016/0012-821X(87)90151-8
[5]   The Argon constraints on mantle structure. [J].
Allegre, CJ ;
Hofmann, A ;
ONions, K .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (24) :3555-3557
[6]   PREDICTION OF CRYSTAL-MELT PARTITION-COEFFICIENTS FROM ELASTIC-MODULI [J].
BLUNDY, J ;
WOOD, B .
NATURE, 1994, 372 (6505) :452-454
[7]  
Blundy J, 2003, EARTH PLANET SC LETT, V210, P383, DOI [10.1016/S0012-821X(03)00129-8, 10.1016/S0012-821X(03)-00129-8]
[8]   SOME THERMODYNAMIC ASPECTS OF GROWTH OF STRAINED CRYSTALS [J].
BRICE, JC .
JOURNAL OF CRYSTAL GROWTH, 1975, 28 (02) :249-253
[9]   SOLUBILITY AND PARTITIONING OF NE, AR, KR, AND XE IN MINERALS AND SYNTHETIC BASALTIC MELTS [J].
BROADHURST, CL ;
DRAKE, MJ ;
HAGEE, BE ;
BERNATOWICZ, TJ .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1992, 56 (02) :709-723
[10]   SOLUBILITY AND PARTITIONING OF AR IN ANORTHITE, DIOPSIDE, FORSTERITE, SPINEL, AND SYNTHETIC BASALTIC LIQUIDS [J].
BROADHURST, CL ;
DRAKE, MJ ;
HAGEE, BE ;
BERNATOWICZ, TJ .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1990, 54 (02) :299-309