Dynamical Processes at the Ice-Water Interface During Solidification

Abstract The dynamics of the freezing process is studied at the surface of growing ice crystal by means of Rayleigh spectroscopy. Light is scattered quasi-elastically at the interface. The line width is proportional to the square of the scattering vector. For a scattering angle of 90° one measure, a...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Bilgram, J. H., Güttinger, H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000033669
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033669
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spelling crcambridgeupr:10.1017/s0022143000033669 2024-03-03T08:45:59+00:00 Dynamical Processes at the Ice-Water Interface During Solidification Bilgram, J. H. Güttinger, H. 1978 http://dx.doi.org/10.1017/s0022143000033669 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033669 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 537-545 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033669 2024-02-08T08:47:47Z Abstract The dynamics of the freezing process is studied at the surface of growing ice crystal by means of Rayleigh spectroscopy. Light is scattered quasi-elastically at the interface. The line width is proportional to the square of the scattering vector. For a scattering angle of 90° one measure, about 2 krad/s. The line width does not depend on the growth rate or thermal gradients at the interface. Light is scattered isotropically, which indicates that the correlation length is small compared with the wavelength of the scattered light. The intensity depends on the growth rate and shows a hysteresis in that dependence; at a minimum growth rate one observes the onset of fluctuations. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 537 545
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Bilgram, J. H.
Güttinger, H.
Dynamical Processes at the Ice-Water Interface During Solidification
topic_facet Earth-Surface Processes
description Abstract The dynamics of the freezing process is studied at the surface of growing ice crystal by means of Rayleigh spectroscopy. Light is scattered quasi-elastically at the interface. The line width is proportional to the square of the scattering vector. For a scattering angle of 90° one measure, about 2 krad/s. The line width does not depend on the growth rate or thermal gradients at the interface. Light is scattered isotropically, which indicates that the correlation length is small compared with the wavelength of the scattered light. The intensity depends on the growth rate and shows a hysteresis in that dependence; at a minimum growth rate one observes the onset of fluctuations.
format Article in Journal/Newspaper
author Bilgram, J. H.
Güttinger, H.
author_facet Bilgram, J. H.
Güttinger, H.
author_sort Bilgram, J. H.
title Dynamical Processes at the Ice-Water Interface During Solidification
title_short Dynamical Processes at the Ice-Water Interface During Solidification
title_full Dynamical Processes at the Ice-Water Interface During Solidification
title_fullStr Dynamical Processes at the Ice-Water Interface During Solidification
title_full_unstemmed Dynamical Processes at the Ice-Water Interface During Solidification
title_sort dynamical processes at the ice-water interface during solidification
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s0022143000033669
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033669
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 537-545
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000033669
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 537
op_container_end_page 545
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