X-ray study of SnO2under high pressure and temperature generated with sintered diamond anvils

Abstract

In-situ X-ray diffraction technique using synchrotron radiation was applied for polymorphic transitions in SnO₂ under high pressure and temperature generated with 6–8 type double-stage multianvils made of sintered diamond. At 23.6 GPa, the mixed phases of rutile-type structure (R-SnO₂) and columbite-type (c-SnO₂) were heated: at 700°C peaks of fluorite-type structure (F-SnO₂) began to appear, and at 1000°C, C-SnO₂ and 5m later R-SnO₂ disappeared completely and a single phase of F-SnO₂ was recognized, indicating a direct transition from R-SnO₂ to F-SnO₂. The volume reduction of 5.3% was obtained for C-SnO₂→F-SnO₂ transition.