An <i>in situ</i> Raman study on katoite Ca<sub>3</sub>Al<sub>2</sub>(O<sub>4</sub>H<sub>4</sub>)<sub>3</sub> at high pressure

DOI
  • 興野 純
    Graduate School of Life and Environmental Sciences, University of Tsukuba
  • Kato Masato
    Graduate School of Life and Environmental Sciences, University of Tsukuba

説明

We report in situ high-pressure Raman spectroscopic study of katoite in a diamond-anvil cell under hydrostatic conditions from 1.3 to 8.3 GPa at room temperature. Three Raman bands at 332, 537 and 3652 cm-1 were observed continuously up to 8.3 GPa. The most striking characteristic was that above 5.1 GPa the pressure derivative of the O-H stretching vibration of F2g symmetry started to decrease significantly. The result leads to a proof that the phase transition of katoite to the high-pressure phase occurs at around 5 GPa.

収録刊行物

キーワード

詳細情報 詳細情報について

  • CRID
    1390846609793655424
  • NII論文ID
    130007786163
  • DOI
    10.14824/jakoka.2018.0_93
  • 本文言語コード
    ja
  • データソース種別
    • JaLC
    • CiNii Articles
  • 抄録ライセンスフラグ
    使用不可

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