کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4742230 1641574 2009 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Aluminum diffusion and Al-vacancy association in periclase
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فیزیک زمین (ژئو فیزیک)
پیش نمایش صفحه اول مقاله
Aluminum diffusion and Al-vacancy association in periclase
چکیده انگلیسی

Trivalent cations in periclase are attracted to cation vacancies and these defects tend to associate on adjacent sites to form mobile pairs. A theory has been developed to describe the concentration-dependent diffusion of Al in the presence of Al-vacancy pairs, and has been applied to experiments conducted at 1577–2273 K and 1 atm to 25 GPa. In all but one experiment, the Gibbs free energy of binding, inferred from the diffusion profiles, is between −44 and −60 kJ/mol, with an average value of −50 kJ/mol. The absolute value of the entropy of binding is constrained to be less than 50 J mol−1 K−1, and the volume of binding is constrained to be between −1.8 and 0 cm3/mol. The diffusion coefficient of the Al-vacancy pair can be described by the equation D2 = D2,0 exp(−(E + PV)/RT), with E = 213 ± 32 kJ/mol, V = 3.22 ± 0.25 cm3/mol, and log10D2,0 = −6.17 ± 0.99 (in m2/s; all uncertainties 2σ). Calculations are presented for the diffusion of Al and Mg as functions of Al concentration, temperature and pressure.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Physics of the Earth and Planetary Interiors - Volume 172, Issues 1–2, January 2009, Pages 34–42
نویسندگان
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