TY - JOUR
T1 - Growth of large (1 mm) MgSiO3 perovskite single crystals
T2 - A thermal gradient method at ultrahigh pressure
AU - Shatskiy, Anton
AU - Fukui, Hiroshi
AU - Matsuzaki, Takuya
AU - Shinoda, Keiji
AU - Yoneda, Akira
AU - Yamazaki, Daisuke
AU - Ito, Eiji
AU - Katsura, Tomoo
PY - 2007/10
Y1 - 2007/10
N2 - Large single crystals of MgSiO3 perovskite were successfully synthesized by a thermal gradient method at 24 GPa and 1500 °C. This was achieved by an improvement of high-pressure synthesis technique that allowed us to grow single crystals under such ultrahigh-pressure conditions in relatively large volumes (e.g., 10 mm3). Since crystal growth is hindered by neighboring crystals, the nucleation density was suppressed by reducing the thermal gradient to 20 °C/mm, permitting an increase in free space for large crystal growth. KHCO3-Mg(OH)2 solvent can be used to grow perovskite crystals. However, the carbonate solvent produces melt inclusions. Silicate sources with MgSiO3 composition produce stishovite inclusions, which in turn cause splitting of perovskite crystals. The formation of these inclusions is avoided by using H2O as a solvent and 85MgSiO3-15Mg2SiO4 as a silicate source. The H2O also allows homogeneous crystal growth, probably because of its low viscosity and high silicate solubility. High-quality single crystals larger than 1 mm were successfully synthesized through these technical developments.
AB - Large single crystals of MgSiO3 perovskite were successfully synthesized by a thermal gradient method at 24 GPa and 1500 °C. This was achieved by an improvement of high-pressure synthesis technique that allowed us to grow single crystals under such ultrahigh-pressure conditions in relatively large volumes (e.g., 10 mm3). Since crystal growth is hindered by neighboring crystals, the nucleation density was suppressed by reducing the thermal gradient to 20 °C/mm, permitting an increase in free space for large crystal growth. KHCO3-Mg(OH)2 solvent can be used to grow perovskite crystals. However, the carbonate solvent produces melt inclusions. Silicate sources with MgSiO3 composition produce stishovite inclusions, which in turn cause splitting of perovskite crystals. The formation of these inclusions is avoided by using H2O as a solvent and 85MgSiO3-15Mg2SiO4 as a silicate source. The H2O also allows homogeneous crystal growth, probably because of its low viscosity and high silicate solubility. High-quality single crystals larger than 1 mm were successfully synthesized through these technical developments.
KW - Growth from solution
KW - High pressure
KW - MgSiO
KW - Perovskite
KW - Single-crystal growth
KW - Temperature gradient method
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U2 - 10.2138/am.2007.2415
DO - 10.2138/am.2007.2415
M3 - Article
AN - SCOPUS:35448947290
SN - 0003-004X
VL - 92
SP - 1744
EP - 1749
JO - American Mineralogist
JF - American Mineralogist
IS - 10
ER -