Proton-containing defects at forsterite {010} tilt grain boundaries and stepped surfaces

被引:41
作者
de Leeuw, NH
Parker, SC
Catlow, CRA
Price, GD
机构
[1] Univ Bath, Sch Chem, Bath BA2 7AY, Avon, England
[2] UCL Royal Inst Great Britain, Davy Faraday Res Lab, London W1X 4BS, England
[3] UCL, Dept Geol Sci, London WC1E 6BT, England
关键词
D O I
10.2138/am-2000-8-904
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 simulation techniques are used to investigate the effect of proton-containing defects on the structure and stabilities of a range of grain boundaries of forsterite. We study two series of stepped {010} tilt boundaries that are at 90 degrees to each other: one with the {100} plane as step wall and the other with the {001} plane. Each series consist of several grain boundaries with increasing terrace area (i.e., decreasing boundary angle). The ratios of boundary and surface energies gamma(b)/gamma(s), and gamma(b)/gamma({010}) with boundary angle show maxima at a boundary angle phi = similar to 30 degrees and minima at phi = 0 degrees and similar to 60 degrees. The adhesion energies of the two series show a minimum at low boundary angle (phi = 20-30 degrees), indicating that there is an optimum size for the (010) terrace area, where the relative stabilities of grain boundary and related surface make separation of the boundary into the free surfaces energetically least expensive. Dissociative adsorption of water molecules in the bulk crystal is preferred at the M2 site, but is an endothermic process with a calculated hydration energy of +119 kJ/mol. Hydration of the grain boundaries on the other hand is energetically favorable with hydration energies tending toward -80 kJ/mol compared with a surface hydration energy at the planar {010} surface of -90 kJ/mol. We also investigated the adsorption of protons at cation defects, by modeling the process of replacement of Mg ions in the bulk and along the grain boundaries by two H(+) ions each. Replacement of Mg(2+) in the bulk crystal occurs preferentially at the MI site and is calculated to be exothermic with a replacement energy of -78 kJ/mol; Mg(2+) replacement along both series of grain boundaries is also an exothermic process. The replacement energies tend to a constant value of approximately -210 kJ/mol with increasing terrace area. (cf., the calculated value for the planar {010} surface of -230.4 kJ/mol).
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页码:1143 / 1154
页数:12
相关论文
共 54 条
[1]  
[Anonymous], 1982, Some Thermodynamic Aspects of Inorganic Chemistry Cambridge
[2]   Atomistic simulation of hydroxide ions in inorganic solids [J].
Baram, PS ;
Parker, SC .
PHILOSOPHICAL MAGAZINE B-PHYSICS OF CONDENSED MATTER STATISTICAL MECHANICS ELECTRONIC OPTICAL AND MAGNETIC PROPERTIES, 1996, 73 (01) :49-58
[3]  
BERAN A, 1999, MICROSCOPIC PROPERTI
[4]  
Born M., 1954, DYNAMICAL THEORY CRY
[5]   COMPUTER MODELING OF SOLID-STATE INORGANIC MATERIALS [J].
CATLOW, CRA ;
PRICE, GD .
NATURE, 1990, 347 (6290) :243-248
[6]  
Dana E. S., 1941, TXB MINERALOGY
[7]   Modelling the effect of water on the surface structure and stability of forsterite [J].
de Leeuw, NH ;
Parker, SC ;
Catlow, CRA ;
Price, GD .
PHYSICS AND CHEMISTRY OF MINERALS, 2000, 27 (05) :332-341
[8]   Computer simulation of dissociative adsorption of water on CaO and MgO surfaces and the relation to dissolution [J].
de Leeuw, NH ;
Parker, SC .
RESEARCH ON CHEMICAL INTERMEDIATES, 1999, 25 (02) :195-211
[9]   Modeling the surface structure and stability of α-quartz [J].
de Leeuw, NH ;
Higgins, FM ;
Parker, SC .
JOURNAL OF PHYSICAL CHEMISTRY B, 1999, 103 (08) :1270-1277
[10]   Molecular-dynamics simulation of MgO surfaces in liquid water using a shell-model potential for water [J].
de Leeuw, NH ;
Parker, SC .
PHYSICAL REVIEW B, 1998, 58 (20) :13901-13908