Small Charged Water Clusters:  Cations

Nonempiric calculation (MP2/UHF/4-31++G**) shows the presence of inherent H3O and OH fragments in small water cluster cations. According to the arrangement of these fragments, the structures of cations are divided into two groups:  either OH fragment acts exclusively as a proton acceptor in all its...

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Published inThe journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory Vol. 103; no. 17; pp. 3285 - 3288
Main Authors Novakovskaya, Yulia V, Stepanov, Nikolai F
Format Journal Article
LanguageEnglish
Published American Chemical Society 29.04.1999
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Summary:Nonempiric calculation (MP2/UHF/4-31++G**) shows the presence of inherent H3O and OH fragments in small water cluster cations. According to the arrangement of these fragments, the structures of cations are divided into two groups:  either OH fragment acts exclusively as a proton acceptor in all its hydrogen bonds, or it is directly bonded to H3O and acts also as a proton donor in the H-bond with a water molecule. At the external effect of about 0.4 eV, the former cations can dissociate into free or quasifree OH radical and a protonated water cluster of the corresponding size. An extrapolation of the adiabatic ionization potentials of water clusters to an infinite cluster size provides the value of 8.5 eV close to the experimental photoelectric threshold of amorphous ice. When the adiabatic hydration of the electron knocked out is taken into account, the energy of 6.8 eV should be sufficient for the ionization of an ice specimen.
Bibliography:ark:/67375/TPS-FNDM679V-T
istex:15B72570D28E3FAD800197372C5199D0B16F26D8
ISSN:1089-5639
1520-5215
DOI:10.1021/jp982982o