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

dc.contributor.authorBekkiyev A.Y.
dc.contributor.authorGlushkov S.M.
dc.contributor.authorZalikhanov M.Ch.
dc.contributor.authorPanchishin I.M.
dc.contributor.authorFadeyev V.V.
dc.contributor.authorUshakova L.A.
dc.contributor.authorKlevtsov A.M.
dc.date.accessioned2020-04-16T07:06:00Z
dc.date.available2020-04-16T07:06:00Z
dc.date.issued1988
dc.description.abstractThis 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.identifierhttps://elibrary.ru/item.asp?id=31020309
dc.identifier.citationTRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 303, 6, 11-13
dc.identifier.issn0891-5571
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/16854
dc.titleUSE OF RAMAN SPECTROSCOPY TO DETERMINE THE LIQUID WATER CONTENT OF SNOW
dc.typeСтатья

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