Observations of ice-crushing phenomena under a skate blade

Experiments using a mock ice-skating blade have shown that when the blade is sliding laterally on an ice surface at 30 mm/s, similar to a skater applying a pushing stride to accelerate or when stopping, crushing produces regular spallation events at the intactice/blade interface (where pressure is ~...

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Bibliographic Details
Main Author: Gagnon, Robert
Format: Article in Journal/Newspaper
Language:English
Published: [Arctic Research Consortium of the U.S.] 2021
Subjects:
Online Access:https://nrc-publications.canada.ca/eng/view/ft/?id=e40b48df-e9dc-4d20-b21d-b2760d101301
https://nrc-publications.canada.ca/eng/view/object/?id=e40b48df-e9dc-4d20-b21d-b2760d101301
https://nrc-publications.canada.ca/fra/voir/objet/?id=e40b48df-e9dc-4d20-b21d-b2760d101301
Description
Summary:Experiments using a mock ice-skating blade have shown that when the blade is sliding laterally on an ice surface at 30 mm/s, similar to a skater applying a pushing stride to accelerate or when stopping, crushing produces regular spallation events at the intactice/blade interface (where pressure is ~50 MPa) that result in a cyclic load pattern (spalling frequency ~ 85 Hz). During forward gliding there was also evidence of spallation events at the gently-upturned ‘bow’ of the blade (spalling frequency ~ 39 Hz). From the speed and force data, and the depths of the lateral shaving and the forward gliding track profile, the energy consumed per unit volume of ice removed was determined in both cases. The energy budget implied that 12% of the shaved ice material was liquid melt, and 18% of the thin sheet-like slurry of liquid and ice particles (< 0.1 mm thickness) extruding from the edges of the blade-bow during gliding was melt. More energy per unit volume was consumed in the gliding case because all spallation debris at the bow was removed from the track by highpressure compaction imposed by the over-running blade. This caused further pulverization and inter-particle ice-on-ice crushing generating mobile slurry that augmented slurry produced on intact-ice hard-zone areas at the blade-ice interface. In the lateral shaving case less material was converted to slurry because many unconfined pieces of the shattered spalls were not subjected to further pulverization/extrusion. This was evident from the post-test observation of the accumulated shaved material that showed spall debris mixed with refrozen extruded slurry. The crushing of ice and presence of slurry under a skate blade are important observations because earlier ice crushing-friction experiments have shown that a thin (< 0.2 mm) highly-lubricating slurry (~16 % liquid) is produced at high-pressure hard-zone contact regions, which facilitates extremely low friction. Peer reviewed: Yes NRC publication: Yes