日本地球惑星科学連合2014年大会

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セッション記号 M (領域外・複数領域) » M-TT 計測技術・研究手法

[M-TT42_2AM1] 地球化学の最前線:先端的手法から探る地球像

2014年5月2日(金) 09:00 〜 10:50 314 (3F)

コンビーナ:*横山 祐典(東京大学 大気海洋研究所 海洋底科学部門/地球表層圏変動研究センター)、鍵 裕之(東京大学大学院理学系研究科附属地殻化学実験施設)、橘 省吾(北海道大学大学院理学研究院自然史科学専攻地球惑星システム科学分野)、平田 岳史(京都大学大学院理学研究科地球惑星科学専攻)、角皆 潤(名古屋大学大学院環境学研究科)、鈴木 勝彦(独立行政法人海洋研究開発機構・地球内部ダイナミクス領域)、下田 玄(産業技術総合研究所地質調査総合センター)、角野 浩史(東京大学大学院理学系研究科附属地殻化学実験施設)、小畑 元(東京大学大気海洋研究所海洋化学部門海洋無機化学分野)、高橋 嘉夫(広島大学大学院理学研究科地球惑星システム学専攻)、横山 哲也(東京工業大学大学院理工学研究科地球惑星科学専攻)、座長:横山 祐典(東京大学 大気海洋研究所 海洋底科学部門/地球表層圏変動研究センター)、橘 省吾(北海道大学大学院理学研究院自然史科学専攻地球惑星システム科学分野)、鍵 裕之(東京大学大学院理学系研究科附属地殻化学実験施設)

09:15 〜 09:30

[MTT42-02] 水圏での金属イオンのスペシエーション: 多種の酸素配位配位子の比較

*高橋 嘉夫1宮地 亜沙美1田中 雅人1 (1.広島大学大学院理学研究科)

キーワード:スペシエーション, エントロピー, 錯生成, 加水分解, 量子化学計算

Complexation of metal cations with ligands such as hydroxide ion, carbonate ion, carboxylate ion, and phosphate ion is one of the most important factors controlling behaviors of metal ions in natural environment. Previous studies showed that these ligands were classified as "intermediate hard ligands" having oxygen donor, which favors to form ionic bonding. However, it was found that the reactivity of these ligands depends on ionic radius and that there is a difference of the reactivity between hydroxide ion and other intermediate hard ligands such as carbonate and carboxylate. For example, among divalent alkaline earth metal ions, Mg2+ mainly precipitates as hydroxide (brucite), while Ca2+ prefers to form carbonate (calcite) or phosphate (apatite) minerals rather than hydroxide. However, quantitative discussion on the selectivity of metal cations has not been performed. In this study, we evaluated the standard Gibbs free energy, entropy, and enthalpy for the complex formation of hydrated metal cations with these ligands based on a critical thermodynamic database. As a result, we found that the entropic contribution to the free energy was large in the case of hydroxide complex of smaller cation. In contrast, the entropic contribution to the free energy was small in the case of hydroxide complex of larger cation and other complexes. In addition, the enthalpy contribution was not significant in this reaction. In the aqueous complexation reaction, entropy was controlled by the number of water molecules replaced by the ligand, suggesting that hydroxide complex for large cation was not stable due to the small effect of dehydration. This suggestion was confirmed by quantum mechanical calculations, which was performed with B3LYP/6-311+G* level using Gaussian 09. We calculated distance between metal (M) in the center and oxygen (O) in the ligand with the increase of number of water molecules placed in the vicinity of the metal ion. As a result, it was found that the M-O distance for hydroxide complex is larger than that of carbonate in the case of larger cation and vice versa This means that hydroxide prefers to form outer-sphere complex for lager metal ion, which is not the case of other intermediate hard ligands. This result is consistent with what we suggested based on the thermodynamic data.