USE OF RAMAN SPECTROSCOPY TO DETERMINE THE LIQUID WATER CONTENT OF SNOW

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dc.contributor.author Bekkiyev A.Y.
dc.contributor.author Glushkov S.M.
dc.contributor.author Zalikhanov M.Ch.
dc.contributor.author Panchishin I.M.
dc.contributor.author Fadeyev V.V.
dc.contributor.author Ushakova L.A.
dc.contributor.author Klevtsov A.M.
dc.date.accessioned 2020-04-16T07:06:00Z
dc.date.available 2020-04-16T07:06:00Z
dc.date.issued 1988
dc.identifier https://elibrary.ru/item.asp?id=31020309
dc.identifier.citation TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 303, 6, 11-13
dc.identifier.issn 0891-5571
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/16854
dc.description.abstract This article shows Raman spectra of water in the liquid (a) and solid (b) states. There are considerable differences between these spectra. We have made a detailed study of the alteration of the spectra when water crystallizes, using various types of excitation and measurement of the spectra. With a 180° recording geometry, the Raman spectrum of a two-phase mixture (solid and liquid) represents a superposition of the spectra of water and ice. A direct consequence of this is the conclusion that it may be possible to determine the partial volumes of the two phases in the mixture. We used a device in which the Raman spectrometer recorded radiation backscattered 180° relative to the exciting radiation at the Stokes frequencies, and a 300 mW LG-106M-1 argon laser operating at 488 nm. We obtained high-quality Raman spectra from the surface of freshly fallen snow.
dc.title USE OF RAMAN SPECTROSCOPY TO DETERMINE THE LIQUID WATER CONTENT OF SNOW
dc.type Статья


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