In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea Ice

The kinetic coefficient of friction μk was measured for sea ice, stainless steel, and coated steel sliding on a natural sea ice cover. The effects of normal stress (3.10–8.11 kPa), ice columnar grain orientation (vertical and parallel to the sliding direction), sliding velocity (0.02–2.97 m·s–1), an...

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Published in:Applied Sciences
Main Authors: Qingkai Wang, Zhijun Li, Peng Lu, Xiaowei Cao, Matti Leppäranta
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/app8050675
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spelling ftmdpi:oai:mdpi.com:/2076-3417/8/5/675/ 2023-08-20T04:09:42+02:00 In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea Ice Qingkai Wang Zhijun Li Peng Lu Xiaowei Cao Matti Leppäranta agris 2018-04-26 application/pdf https://doi.org/10.3390/app8050675 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/app8050675 https://creativecommons.org/licenses/by/4.0/ Applied Sciences; Volume 8; Issue 5; Pages: 675 sea ice kinetic friction coefficient in situ test sliding velocity ice navigation Text 2018 ftmdpi https://doi.org/10.3390/app8050675 2023-07-31T21:29:41Z The kinetic coefficient of friction μk was measured for sea ice, stainless steel, and coated steel sliding on a natural sea ice cover. The effects of normal stress (3.10–8.11 kPa), ice columnar grain orientation (vertical and parallel to the sliding direction), sliding velocity (0.02–2.97 m·s–1), and contact material were investigated. Air temperature was higher than −5.0 °C for the test duration. The results showed a decline of μk with increasing normal stress with μk independent of ice grain orientation. The μk of different materials varied, partly due to distinct surface roughnesses, but all cases showed a similar increasing trend with increasing velocity because of the viscous resistance of melt-water film. The velocity dependence of μk was quantified using the rate- and state- dependent model, and μk was found to increase logarithmically with increasing velocity. In addition, μk obtained at higher air temperatures was greater than at lower temperatures. The stick-slip phenomenon was observed at a relatively high velocity compared with previous studies, which was partly due to the low-stiffness device used in the field. Based on the experimental data, the calculation of physical models can be compared. Text Sea ice MDPI Open Access Publishing Applied Sciences 8 5 675
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic sea ice
kinetic friction coefficient
in situ test
sliding velocity
ice navigation
spellingShingle sea ice
kinetic friction coefficient
in situ test
sliding velocity
ice navigation
Qingkai Wang
Zhijun Li
Peng Lu
Xiaowei Cao
Matti Leppäranta
In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea Ice
topic_facet sea ice
kinetic friction coefficient
in situ test
sliding velocity
ice navigation
description The kinetic coefficient of friction μk was measured for sea ice, stainless steel, and coated steel sliding on a natural sea ice cover. The effects of normal stress (3.10–8.11 kPa), ice columnar grain orientation (vertical and parallel to the sliding direction), sliding velocity (0.02–2.97 m·s–1), and contact material were investigated. Air temperature was higher than −5.0 °C for the test duration. The results showed a decline of μk with increasing normal stress with μk independent of ice grain orientation. The μk of different materials varied, partly due to distinct surface roughnesses, but all cases showed a similar increasing trend with increasing velocity because of the viscous resistance of melt-water film. The velocity dependence of μk was quantified using the rate- and state- dependent model, and μk was found to increase logarithmically with increasing velocity. In addition, μk obtained at higher air temperatures was greater than at lower temperatures. The stick-slip phenomenon was observed at a relatively high velocity compared with previous studies, which was partly due to the low-stiffness device used in the field. Based on the experimental data, the calculation of physical models can be compared.
format Text
author Qingkai Wang
Zhijun Li
Peng Lu
Xiaowei Cao
Matti Leppäranta
author_facet Qingkai Wang
Zhijun Li
Peng Lu
Xiaowei Cao
Matti Leppäranta
author_sort Qingkai Wang
title In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea Ice
title_short In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea Ice
title_full In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea Ice
title_fullStr In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea Ice
title_full_unstemmed In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea Ice
title_sort in situ experimental study of the friction of sea ice and steel on sea ice
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/app8050675
op_coverage agris
genre Sea ice
genre_facet Sea ice
op_source Applied Sciences; Volume 8; Issue 5; Pages: 675
op_relation https://dx.doi.org/10.3390/app8050675
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/app8050675
container_title Applied Sciences
container_volume 8
container_issue 5
container_start_page 675
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