日本地球惑星科学連合2018年大会

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[JJ] 口頭発表

セッション記号 S (固体地球科学) » S-MP 岩石学・鉱物学

[S-MP38] 鉱物の物理化学

2018年5月24日(木) 10:45 〜 12:15 A04 (東京ベイ幕張ホール)

コンビーナ:大藤 弘明(愛媛大学地球深部ダイナミクス研究センター)、鎌田 誠司(東北大学学際科学フロンティア研究所)、座長:大藤 弘明

11:30 〜 11:45

[SMP38-10] Cijs of single crystal Pt under high pressure based on IXS and primary pressure scale

*鎌田 誠司1,2福井 宏之3,4米田 明5前田 郁也2筒井 智嗣6内山 裕士4,6平尾 直久6石川 大介6バロン アルフレッド4 (1.東北大学学際科学フロンティア研究所、2.東北大学大学院理学研究科地学専攻、3.兵庫県立大学大学院物質理学研究科、4.理化学研究所物質ダイナミクス研究室、5.岡山大学惑星物質研究所、6.高輝度光科学研究センター)

キーワード:単結晶弾性、白金一次圧力スケール、非弾性X線散乱法、ダイヤモンドアンビルセル

There have been conflicts between previously proposed equations of state of platinum (Pt) in spite of importance of precise pressures under high pressure conditions. In order to determine independently EOS, the elastic constants of Pt, C11, C12, and C44, were obtained based on inelastic X-ray scattering from ambient condition to ca. 20 GPa. The lattice parameters under high pressure conditions were measured simultaneously. Adiabatic bulk moduli and shear moduli were obtained from Cijs and experimental pressures were calculated by integrating KT(V). The EOS of Pt as a primary pressure scale was determined based on the experimental pressures. The pressures by our scale are 5 to 10 % lower than those of previous studies up to 200 GPa. Above 200 GPa, the present pressure scale shows up to 5 % higher pressures than pressures by the scales determined by XRD. On the other hand, our pressure scale shows 10 % lower pressures than those by the scales determined by shock data. In addition, the pressures based on the current scale show a good agreement those by Au scale obtained the same method, when pressures are calculated by using volumes of Pt and Au obtained simultaneously up to 140 GPa. On the other hand, the difference between pressures by previous Pt and Au scales become remarkable above 100 GPa.