Pressure responses of portlandite and H-D isotope effects on pressure-induced phase transitions

ポートランダイトにおける圧力応答と圧力誘起相転移に関する同位体効果

飯塚 理子*; 鍵 裕之*; 小松 一生*; 牛嶋 大地*; 中野 智志*; 佐野 亜沙美   ; 永井 隆哉*; 八木 健彦*

Iizuka, Riko*; Kagi, Hiroyuki*; Komatsu, Kazuki*; Ushijima, Daichi*; Nakano, Satoshi*; Sano, Asami; Nagai, Takaya*; Yagi, Takehiko*

含水鉱物ポートランダイト(Ca(OH))の高圧下におけるラマンスペクトル,IRスペクトル及びX線回折実験を行った。ラマンスペクトル,IRスペクトルの測定では、Ca(OH)では高圧相への相転移がCa(OD)よりも低圧でおき、相転移圧力には同位体による違いがあった。X線回折実験では高圧相が28.5GPaまで安定に存在し、以前報告のあったアモルファス化は静水圧条件下では見られないことが明らかになった。

The pressure responses of portlandite and the isotope effect on the phase transition were investigated at room temperature from single-crystal Raman and IR spectra and from powder X-ray diffraction using diamond anvil cells under quasi-hydrostatic conditions in a helium pressure-transmitting medium. Phase transformation and subsequent peak broadening observed from the Raman and IR spectra of Ca(OH) occurred at lower pressures than those of Ca(OD). In contrast, no isotope effect was found on the volume and axial compressions observed from powder X-ray diffraction patterns. X-ray diffraction lines attributable to the high-pressure phase remained up to 28.5 GPa, suggesting no total amorphization in a helium pressure medium within the examined pressure region. These results suggest that the H-D isotope effect is engendered in the local environment surrounding H(D) atoms.