1989
DOI: 10.1070/qe1989v019n04abeh007918
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Raman scattering spectra recorded in the course of the water–ice phase transition and laser diagnostics of heterophase water systems

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Cited by 3 publications
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“…Further, for liquid water, the isotropic component of the polarized Raman spectrum dominates at 3000−3300 cm -1 , consistent with water in a symmetrical environment. The resonance at 3300−3600 cm -1 is a convolution of at least two resonances: both the OH stretch of water in an asymmetrical environment and the asymmetric stretch of water in a symmetrical environment contribute to this band. ,,, Water in the first layer of the interface necessarily has disrupted tetrahedral bonding; however, due to the similarity to the bulk water hydrogen-bonded spectrum, the following assignments are generally used. The peak at 3700 cm -1 is assigned to an OH stretch free of hydrogen bonding reflecting the disrupted tetrahedral bonding at the surface.…”
Section: Discussionmentioning
confidence: 99%
“…Further, for liquid water, the isotropic component of the polarized Raman spectrum dominates at 3000−3300 cm -1 , consistent with water in a symmetrical environment. The resonance at 3300−3600 cm -1 is a convolution of at least two resonances: both the OH stretch of water in an asymmetrical environment and the asymmetric stretch of water in a symmetrical environment contribute to this band. ,,, Water in the first layer of the interface necessarily has disrupted tetrahedral bonding; however, due to the similarity to the bulk water hydrogen-bonded spectrum, the following assignments are generally used. The peak at 3700 cm -1 is assigned to an OH stretch free of hydrogen bonding reflecting the disrupted tetrahedral bonding at the surface.…”
Section: Discussionmentioning
confidence: 99%
“…The technique, as employed has been reported in detail [2]. The first series of experiments was carried out employing a specially developed optical cryogenic technique.…”
Section: A Experimental and Instrumentationmentioning
confidence: 99%