Application of a new friction theory to ice and snow
A new theory, in which friction is interpreted as the energy flux required to form surface at contact asperities, is applied to sliding on ice and snow. The results of this theoretical investigation show that in dry friction the relevant contact areas are of almost molecular scale. The properties of...
Published in: | Annals of Glaciology |
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1994
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Online Access: | https://cris.vtt.fi/en/publications/4be181be-3f9c-451a-aef1-6baa477755ee https://doi.org/10.3189/1994AoG19-1-155-157 |
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ftvttcrispub:oai:cris.vtt.fi:publications/4be181be-3f9c-451a-aef1-6baa477755ee 2023-05-15T13:29:19+02:00 Application of a new friction theory to ice and snow Makkonen, Lasse 1994 https://cris.vtt.fi/en/publications/4be181be-3f9c-451a-aef1-6baa477755ee https://doi.org/10.3189/1994AoG19-1-155-157 eng eng info:eu-repo/semantics/closedAccess Makkonen , L 1994 , ' Application of a new friction theory to ice and snow ' , Annals of Glaciology , vol. 19 , pp. 155-157 . https://doi.org/10.3189/1994AoG19-1-155-157 article 1994 ftvttcrispub https://doi.org/10.3189/1994AoG19-1-155-157 2022-10-13T13:55:16Z A new theory, in which friction is interpreted as the energy flux required to form surface at contact asperities, is applied to sliding on ice and snow. The results of this theoretical investigation show that in dry friction the relevant contact areas are of almost molecular scale. The properties of the interface layer in ice and snow friction arc poorly known, so that the implications of this new theory are somewhat speculative. However, qualitative agreement with experimental data is good, and the theory provides explanations to the success of some empirically developed methods of improving the frictional properties of skis and sledges. Article in Journal/Newspaper Annals of Glaciology VTT's Research Information Portal Annals of Glaciology 19 155 157 |
institution |
Open Polar |
collection |
VTT's Research Information Portal |
op_collection_id |
ftvttcrispub |
language |
English |
description |
A new theory, in which friction is interpreted as the energy flux required to form surface at contact asperities, is applied to sliding on ice and snow. The results of this theoretical investigation show that in dry friction the relevant contact areas are of almost molecular scale. The properties of the interface layer in ice and snow friction arc poorly known, so that the implications of this new theory are somewhat speculative. However, qualitative agreement with experimental data is good, and the theory provides explanations to the success of some empirically developed methods of improving the frictional properties of skis and sledges. |
format |
Article in Journal/Newspaper |
author |
Makkonen, Lasse |
spellingShingle |
Makkonen, Lasse Application of a new friction theory to ice and snow |
author_facet |
Makkonen, Lasse |
author_sort |
Makkonen, Lasse |
title |
Application of a new friction theory to ice and snow |
title_short |
Application of a new friction theory to ice and snow |
title_full |
Application of a new friction theory to ice and snow |
title_fullStr |
Application of a new friction theory to ice and snow |
title_full_unstemmed |
Application of a new friction theory to ice and snow |
title_sort |
application of a new friction theory to ice and snow |
publishDate |
1994 |
url |
https://cris.vtt.fi/en/publications/4be181be-3f9c-451a-aef1-6baa477755ee https://doi.org/10.3189/1994AoG19-1-155-157 |
genre |
Annals of Glaciology |
genre_facet |
Annals of Glaciology |
op_source |
Makkonen , L 1994 , ' Application of a new friction theory to ice and snow ' , Annals of Glaciology , vol. 19 , pp. 155-157 . https://doi.org/10.3189/1994AoG19-1-155-157 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.3189/1994AoG19-1-155-157 |
container_title |
Annals of Glaciology |
container_volume |
19 |
container_start_page |
155 |
op_container_end_page |
157 |
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1765999932708225024 |