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...

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Bibliographic Details
Published in:Annals of Glaciology
Main Author: Makkonen, Lasse
Format: Article in Journal/Newspaper
Language:English
Published: 1994
Subjects:
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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spelling 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
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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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