日本地球惑星科学連合2018年大会

講演情報

[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) 09:00 〜 10:30 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:鹿山 雅裕(東北大学)

09:15 〜 09:30

[SMP38-02] The failure of DFT and DFT+U on predictions of structural and magnetic properties of epsilon-oxygen

*The Anh Le1Masahiro Wada2Hiroshi Fukui2Toshiaki Iitaka1 (1.RIKEN、2.University of Hyogo)

キーワード:DFT, DFT+U, solid oxygen, epsilon phase

We systematically calculated the structural, magnetic and electronic properties of the epsilon phase of solid oxygen using conventional DFT and DFT+U. While DFT+U can predict the structural epsilon-zeta transition at 80 GPa, which was found at 96 GPa by experiment, conventional DFT calculation only predicts the transition at 50 GPa. On the other hand, conventional DFT shows no magnetic configuration at all pressure above 10 GPa which is consistent with neutron diffraction measurement. The DFT+U predicts the existence of anti-ferromagnetic configuration of the epsilon phase. This talk will discuss the failure of both DFT and DFT+U in comparison with experiments and possible explanations.