2024-03-28T22:06:41Zhttps://eprints.lib.hokudai.ac.jp/dspace-oai/requestoai:eprints.lib.hokudai.ac.jp:2115/58692022-11-17T02:08:08Zhdl_2115_20056hdl_2115_147Adhesion shear theory of ice friction at low sliding velocities, combined with ice sinteringMaeno, NorikazuArakawa, Masahiko423.5Adhesion and shear deformation of ice have been traditionally considered to be responsible for ice friction at sliding velocities lower than about 10–2 m/s, but the simple mechanism cannot explain the recent finding that the ice–ice friction coefficient increases with decreasing sliding velocity. This article proposes an improved adhesion shear theory, which takes account of junction growth of asperities at the sliding ice interface due to sintering. At lower sliding velocities and higher homologous temperatures, contacts of ice asperities develop resulting in the increase of friction force.American Institute of PhysicsJournal Articleapplication/pdfhttp://hdl.handle.net/2115/5869https://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/5869/1/JAP95-1.pdf0021-8979Journal of Applied Physics9511341392004-01enginfo:doi/10.1063/1.1633654Copyright © 2004 American Institute of Physicspublisher