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- W2016354413 abstract "The origin of O−H vibrational red-shifts observed experimentally in (H2 clusters is analyzed using electronic structure calculations, including natural bond orbital analysis. The red-shifts are shown to arise from significant charge transfer and strong donor−acceptor stabilization between the unpaired electron and O−H σ* orbitals on a nearby water molecule in a double hydrogen-bond-acceptor (“AA”) configuration. The extent of e- → σ* charge transfer is comparable to the n → σ* charge transfer in the most strongly hydrogen-bonded X-(H2O) complexes (e.g., X = F, O, OH), even though the latter systems exhibit much larger vibrational red-shifts. In X-(H2O), the proton affinity of X- induces a low-energy XH···-OH diabatic state that becomes accessible in v = 1 of the shared-proton stretch, leading to substantial anharmonicity in this mode. In contrast, the H + -OH(H2O)n-1 diabat of (H2 is not energetically accessible; thus, the O−H stretching modes of the AA water are reasonably harmonic, and their red-shifts are less dramatic. Only a small amount of charge penetrates beyond the AA water molecule, even upon vibrational excitation of these AA modes. Implications for modeling of the aqueous electron are discussed." @default.
- W2016354413 created "2016-06-24" @default.
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- W2016354413 date "2006-10-01" @default.
- W2016354413 modified "2023-10-17" @default.
- W2016354413 title "Charge Penetration and the Origin of Large O−H Vibrational Red-Shifts in Hydrated-Electron Clusters, (H<sub>2</sub>O)<sub><i>n</i></sub><sup>-</sup>" @default.
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- W2016354413 doi "https://doi.org/10.1021/ja064949i" @default.
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