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 (0.0...

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Main Authors: Qingkai Wang, Zhijun Li, Peng Lu, Xiaowei Cao, Matti Leppäranta
Format: Article
Language:English
Published: MDPI AG 2018-04-01
Series:Applied Sciences
Subjects:
Online Access:http://www.mdpi.com/2076-3417/8/5/675
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spelling doaj-58d8d616da0b4ae696069e68708f48b42020-11-25T01:29:28ZengMDPI AGApplied Sciences2076-34172018-04-018567510.3390/app8050675app8050675In Situ Experimental Study of the Friction of Sea Ice and Steel on Sea IceQingkai Wang0Zhijun Li1Peng Lu2Xiaowei Cao3Matti Leppäranta4State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, ChinaState Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, ChinaState Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, ChinaState Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, ChinaInstitute of Atmospheric and Earth Sciences, University of Helsinki, Helsinki FI-00014, FinlandThe 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.http://www.mdpi.com/2076-3417/8/5/675sea icekinetic friction coefficientin situ testsliding velocityice navigation
collection DOAJ
language English
format Article
sources DOAJ
author Qingkai Wang
Zhijun Li
Peng Lu
Xiaowei Cao
Matti Leppäranta
spellingShingle 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
Applied Sciences
sea ice
kinetic friction coefficient
in situ test
sliding velocity
ice navigation
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 MDPI AG
series Applied Sciences
issn 2076-3417
publishDate 2018-04-01
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.
topic sea ice
kinetic friction coefficient
in situ test
sliding velocity
ice navigation
url http://www.mdpi.com/2076-3417/8/5/675
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AT zhijunli insituexperimentalstudyofthefrictionofseaiceandsteelonseaice
AT penglu insituexperimentalstudyofthefrictionofseaiceandsteelonseaice
AT xiaoweicao insituexperimentalstudyofthefrictionofseaiceandsteelonseaice
AT mattilepparanta insituexperimentalstudyofthefrictionofseaiceandsteelonseaice
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