TY - JOUR
T1 - Stishovite single-crystal growth and application to silicon self-diffusion measurements
AU - Shatskiy, Anton
AU - Yamazaki, Daisuke
AU - Borzdov, Yuriy M.
AU - Matsuzaki, Takuya
AU - Litasov, Konstantin D.
AU - Cooray, Titus
AU - Ferot, Anais
AU - Eiji, I. T.O.
AU - Tomoo, Katsura
PY - 2010/1
Y1 - 2010/1
N2 - Large single crystals of stishovite were successfully synthesized at 11 GPa from a silica solution in water. The potential of both slow cooling and thermal gradient methods were examined. The thermal gradient method provided crystals of 0.8 × 0.8 × 1.3 mm in size grown at 1350 °C and a thermal gradient of 50 °C/mm using stishovite as a silica source. The use of quartz: as a source resulted in the appearance of numerous stishovite crystals in the solution interior resulting in diminished space for the growth of large crystals. This can be explained by a significant difference in the solubility of metastable quartz and stishovite in water, estimated to be 85.3 and 5.6 wt% SiO2 at 1000 °C and 11 GPa, respectively. Crystals up to 0.8 × 1.3 × 1.5 mm were grown by the slow cooling method in the system SiO2 + 14.7 wt% H2O as temperature was decreased from 1600 to 1000 °C with a cooling rate of 2 °C/min. The size of single crystals obtained was large enough to carry out silicon self-diffusion experiments, which were performed at a pressure of 14 GPa and temperatures from. 1400 to 1800 °C. The lattice diffusion coefficients along the [110] and [001] directions can be expressed as D[110] (m2/s) = 4.10 × 10 -12 exp [-322 (kJ/mol)/RT] and D[001] (mVs) = 5.62 × 1.0-12 exp [-334 (kJ/mol)/RT], respectively, where R is the gas constant and T is the absolute temperature.
AB - Large single crystals of stishovite were successfully synthesized at 11 GPa from a silica solution in water. The potential of both slow cooling and thermal gradient methods were examined. The thermal gradient method provided crystals of 0.8 × 0.8 × 1.3 mm in size grown at 1350 °C and a thermal gradient of 50 °C/mm using stishovite as a silica source. The use of quartz: as a source resulted in the appearance of numerous stishovite crystals in the solution interior resulting in diminished space for the growth of large crystals. This can be explained by a significant difference in the solubility of metastable quartz and stishovite in water, estimated to be 85.3 and 5.6 wt% SiO2 at 1000 °C and 11 GPa, respectively. Crystals up to 0.8 × 1.3 × 1.5 mm were grown by the slow cooling method in the system SiO2 + 14.7 wt% H2O as temperature was decreased from 1600 to 1000 °C with a cooling rate of 2 °C/min. The size of single crystals obtained was large enough to carry out silicon self-diffusion experiments, which were performed at a pressure of 14 GPa and temperatures from. 1400 to 1800 °C. The lattice diffusion coefficients along the [110] and [001] directions can be expressed as D[110] (m2/s) = 4.10 × 10 -12 exp [-322 (kJ/mol)/RT] and D[001] (mVs) = 5.62 × 1.0-12 exp [-334 (kJ/mol)/RT], respectively, where R is the gas constant and T is the absolute temperature.
UR - http://www.scopus.com/inward/record.url?scp=77249100460&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=77249100460&partnerID=8YFLogxK
U2 - 10.2138/am.2010.3255
DO - 10.2138/am.2010.3255
M3 - Article
AN - SCOPUS:77249100460
SN - 0003-004X
VL - 95
SP - 135
EP - 143
JO - American Mineralogist
JF - American Mineralogist
IS - 1
ER -