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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