An Electron Microscope Study of Snow Crystal Nuclei
Abstract Snow crystals were received on the collodion film of the holder of an electron microscope, and made to sublimate without melting. These specimens were investigated under an electron microscope. One solid nucleus was always observed in the central portion of a snow crystal. These centre nucl...
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Cambridge University Press (CUP)
1953
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Online Access: | http://dx.doi.org/10.1017/s0022143000025661 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025661 |
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crcambridgeupr:10.1017/s0022143000025661 2024-03-03T08:46:00+00:00 An Electron Microscope Study of Snow Crystal Nuclei Nakaya, Ukichiro 1953 http://dx.doi.org/10.1017/s0022143000025661 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025661 en eng Cambridge University Press (CUP) Journal of Glaciology volume 2, issue 13, page 176-180 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1953 crcambridgeupr https://doi.org/10.1017/s0022143000025661 2024-02-08T08:36:10Z Abstract Snow crystals were received on the collodion film of the holder of an electron microscope, and made to sublimate without melting. These specimens were investigated under an electron microscope. One solid nucleus was always observed in the central portion of a snow crystal. These centre nuclei were of sizes between 0.5 and 8 μ . Most of them were presumed to be kaolin, clay or carbon particles; some were considered to be micro-organisms. In the other parts of snow crystals numerous smaller nuclei were observed, whose dimensions were of the order of those of condensation nuclei. These condensation nuclei were found to be of two kinds, the larger ones most frequently having a diameter of about 0.15 μ , the smaller ones of about 0.05 μ . A new theory was proposed from the data of the electron microscopic studies and those of the conditions of formation of snow crystals. In this theory it is proposed that minute water droplets of 1 μ or so play an important rôls in the process of snow crystal growth. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 2 13 176 180 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Nakaya, Ukichiro An Electron Microscope Study of Snow Crystal Nuclei |
topic_facet |
Earth-Surface Processes |
description |
Abstract Snow crystals were received on the collodion film of the holder of an electron microscope, and made to sublimate without melting. These specimens were investigated under an electron microscope. One solid nucleus was always observed in the central portion of a snow crystal. These centre nuclei were of sizes between 0.5 and 8 μ . Most of them were presumed to be kaolin, clay or carbon particles; some were considered to be micro-organisms. In the other parts of snow crystals numerous smaller nuclei were observed, whose dimensions were of the order of those of condensation nuclei. These condensation nuclei were found to be of two kinds, the larger ones most frequently having a diameter of about 0.15 μ , the smaller ones of about 0.05 μ . A new theory was proposed from the data of the electron microscopic studies and those of the conditions of formation of snow crystals. In this theory it is proposed that minute water droplets of 1 μ or so play an important rôls in the process of snow crystal growth. |
format |
Article in Journal/Newspaper |
author |
Nakaya, Ukichiro |
author_facet |
Nakaya, Ukichiro |
author_sort |
Nakaya, Ukichiro |
title |
An Electron Microscope Study of Snow Crystal Nuclei |
title_short |
An Electron Microscope Study of Snow Crystal Nuclei |
title_full |
An Electron Microscope Study of Snow Crystal Nuclei |
title_fullStr |
An Electron Microscope Study of Snow Crystal Nuclei |
title_full_unstemmed |
An Electron Microscope Study of Snow Crystal Nuclei |
title_sort |
electron microscope study of snow crystal nuclei |
publisher |
Cambridge University Press (CUP) |
publishDate |
1953 |
url |
http://dx.doi.org/10.1017/s0022143000025661 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025661 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 2, issue 13, page 176-180 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000025661 |
container_title |
Journal of Glaciology |
container_volume |
2 |
container_issue |
13 |
container_start_page |
176 |
op_container_end_page |
180 |
_version_ |
1792501773718519808 |