Direct evidence of orbital mixing between water and solvated transition-metal ions:: An oxygen 1s XAS and DFT study of aqueous systems

被引:69
作者
Näslund, LÅ
Cavalleri, M
Ogasawara, H
Nilsson, A
Pettersson, LGM [1 ]
Wernet, P
Edwards, DC
Sandström, M
Myneni, S
机构
[1] Stockholm Univ, Arrhenius Lab, Fysikum, SE-10691 Stockholm, Sweden
[2] Uppsala Univ, Dept Phys, SE-75121 Uppsala, Sweden
[3] Stanford Synchrotron Radiat Lab, Stanford, CA 94309 USA
[4] Princeton Univ, Dept Chem, Princeton, NJ 08544 USA
[5] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
关键词
D O I
10.1021/jp034296h
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We have studied the chemical bonding of water in the first hydration sphere to transition-metal ions in aqueous solutions by using X-ray absorption spectroscopy (XAS) combined with density functional theory calculations (DFT). The experimental technique is for the first time applied to the study of the oxygen K-edge absorption of liquid water in the presence of dissolved ions. We successfully resolved the electronic structure of water in the first hydration sphere. Features in the oxygen Is XAS pre-edge region in Cr3+ and Fe3+ solutions are interpreted as mixing between the molecular orbitals of water and the open d shell of the transition-metal ion. These features are absent for Al3+ solutions. Effects on the electronic structure from anions in the first hydration sphere are also described.
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收藏
页码:6869 / 6876
页数:8
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