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[1] Sea ice friction models are necessary to predict the nature of interactions between sea ice floes. These interactions are of interest on a range of scales, for example, to predict loads on engineering structures in icy waters or to understand the basinscale motion of sea ice. Many models use Amo...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.660.2129 2023-05-15T18:17:24+02:00 CentAUR A Rate Ben Lishman Peter Sammonds Danny Feltham The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.660.2129 http://centaur.reading.ac.uk/34651/1/jgrc11768.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.660.2129 http://centaur.reading.ac.uk/34651/1/jgrc11768.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://centaur.reading.ac.uk/34651/1/jgrc11768.pdf text ftciteseerx 2016-01-08T16:50:25Z [1] Sea ice friction models are necessary to predict the nature of interactions between sea ice floes. These interactions are of interest on a range of scales, for example, to predict loads on engineering structures in icy waters or to understand the basinscale motion of sea ice. Many models use Amontons friction law due to its simplicity. More advanced models allow for hydrodynamic lubrication and refreezing of asperities; however, modeling these processes leads to greatly increased complexity. In this paper we propose, by analogy with rock physics, that a rate and statedependent friction law allows us to incorporate memory (and thus the effects of lubrication and bonding) into ice friction models without a great increase in complexity. We support this proposal with experimental data on both the laboratory (∼0.1 m) and ice tank (∼1 m) scale. These experiments show that the effects of static contact under normal load can be incorporated into a friction model. We find the parameters for a firstorder rate and state model to be A = 0.310, B = 0.382, and m0 = 0.872. Such a model then allows us to make predictions about the nature of memory effects in Text Sea ice Unknown |
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[1] Sea ice friction models are necessary to predict the nature of interactions between sea ice floes. These interactions are of interest on a range of scales, for example, to predict loads on engineering structures in icy waters or to understand the basinscale motion of sea ice. Many models use Amontons friction law due to its simplicity. More advanced models allow for hydrodynamic lubrication and refreezing of asperities; however, modeling these processes leads to greatly increased complexity. In this paper we propose, by analogy with rock physics, that a rate and statedependent friction law allows us to incorporate memory (and thus the effects of lubrication and bonding) into ice friction models without a great increase in complexity. We support this proposal with experimental data on both the laboratory (∼0.1 m) and ice tank (∼1 m) scale. These experiments show that the effects of static contact under normal load can be incorporated into a friction model. We find the parameters for a firstorder rate and state model to be A = 0.310, B = 0.382, and m0 = 0.872. Such a model then allows us to make predictions about the nature of memory effects in |
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The Pennsylvania State University CiteSeerX Archives |
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A Rate Ben Lishman Peter Sammonds Danny Feltham |
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A Rate Ben Lishman Peter Sammonds Danny Feltham CentAUR |
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A Rate Ben Lishman Peter Sammonds Danny Feltham |
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A Rate |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.660.2129 http://centaur.reading.ac.uk/34651/1/jgrc11768.pdf |
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Sea ice |
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Sea ice |
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http://centaur.reading.ac.uk/34651/1/jgrc11768.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.660.2129 http://centaur.reading.ac.uk/34651/1/jgrc11768.pdf |
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1766191597686358016 |