Physics
Scientific paper
May 2000
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000pepi..119..299y&link_type=abstract
Physics of the Earth and Planetary Interiors, Volume 119, Issue 3-4, p. 299-309.
Physics
29
Scientific paper
Silicon self-diffusion coefficients in MgSiO3 perovskite were measured under lower mantle conditions. The MgSiO3 perovskite was synthesized and diffusion annealing experiments were conducted at pressure of 25 GPa and temperature of 1673-2073 K using a MA8 type high-pressure apparatus. The diffusion profiles were obtained by secondary ion mass spectrometry. The lattice and grain boundary diffusion coefficients (D1 and Dgb) were determined to be D1 [m2/s]=2.74×10-10 exp(-336 [kJ/mol]/RT) and δDgb [m3/s]=7.12×10-17 exp(-311 [kJ/mol]/RT), respectively, where δ is the width of grain boundary, R is the gas constant and T is the absolute temperature. These diffusion coefficients play a key role for understanding the rheology of the lower mantle.
Kato Taichi
Ohtani Eiji
Toriumi Mitsuhiro
Yamazaki Dai
Yurimoto Hisayoshi
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