日本地球惑星科学連合2016年大会

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セッション記号 S (固体地球科学) » S-MP 岩石学・鉱物学

[S-MP42] 鉱物の物理化学

2016年5月25日(水) 09:00 〜 10:30 301A (3F)

コンビーナ:*興野 純(筑波大学大学院生命環境科学研究科地球進化科学専攻)、大藤 弘明(愛媛大学地球深部ダイナミクス研究センター)、座長:興野 純(筑波大学大学院生命環境科学研究科地球進化科学専攻)

09:15 〜 09:30

[SMP42-02] 密度汎関数法を用いた氷XVの構造の研究

*則竹 史哉1小松 一生1山根 崚1鍵 裕之1 (1.東京大学地殻化学実験施設)

キーワード:氷、密度汎関数法

There are open questions in the study of ice XV, the ordered phase of ice VI. The previous studies give inconsistent results between permittivity measurement (Johari & Whalley, 1976), neutron diffraction study (Saltzmann et al. 2009), and theoretical studies (Kuo & Kuhs, 2006; Knight & Singer, 2005). Permittivity measurements and theoretical study suggest that ice XV is ferroelectric, whereas neutron diffraction study suggests that ice XV is anti-ferroelectric.
To obtain the consistent result, we classified 45 possible hydrogen configurations using a newly developed invariant, and then performed neutron Rietveld analyses and DFT calculations for every 45 possible configurations. The Quantum Espresso (Giannozzi et al. 2009) was used for the DFT calculations (Hohenberg and Kohn, 1964; Kohn and Sham, 1965). Quantum Espresso is a package for the calculation of electronic structure properties using a plain-wave basis set and pseudopotentials. We used Perdew-Burke-Ernzerhof type non-empirical exchange-correlation functionals (Perdew et al, 1996) for this study. PBE type Xc/Corr energy form gives similar energy tendency (del Ben et al., 2014) with approximations from wave function theory such as a MP2 (Head-Gordon et al. 1988) and RPA (Macher et al., 2014). The pseudopotentials are derived using Troullier-Martins Method (Troullier and Martins, 1991). The enthalpies of 45 possible configurations for ice XV were calculated within an unit cell with the kinetic energy cutoff of 70 Ry and the Brillouin zone k mesh of 5 x 5x 6. The cell and atomic parameters were optimized using BFGS quasi-Newton method (Broyden, 1970; Fletcher, 1970; Goldfarb, 1970; Shanno, 1970) at atmospheric pressure. The phonons were calculated using density functional perturbation theory (Baroni et al., 2001). To correct the effect of zero-point motions of atoms, we added calculated phonon energy (=1/2Σnωn) to the enthalpies from structural optimizations for each configuration. The effect of ferro-electricity were corrected by the Ewald construction, the same as the previous work about ice XV (Del Ben et al., 2014).
A consistent result was obtained about the structure of ice XV that the experimentally obtained ice XV have Pmmn space group, that is, the structure of ice XV is partially ordered structure. Our DFT calculations with surface effect corrections suggest that the energy difference between 45 possible patterns is between 0.05 eV (20 K in the reduced temperature). Moreover, the energy differences among several lower energy configurations are within 0.01 eV. Such a small energy difference gives us an interpretation of our experimental result that the ice XV has a Pmmn space group as time-space averaged structure.