A surface topography analysis of the curling stone curl mechanism

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dc.contributor Aalto-yliopisto fi
dc.contributor Aalto University en
dc.contributor.author Honkanen, Viktor
dc.contributor.author Ovaska, Markus
dc.contributor.author Alava, Mikko J.
dc.contributor.author Laurson, Lasse
dc.contributor.author Tuononen, Ari J.
dc.date.accessioned 2018-06-18T09:17:38Z
dc.date.available 2018-06-18T09:17:38Z
dc.date.issued 2018-05-25
dc.identifier.citation Honkanen , V , Ovaska , M , Alava , M J , Laurson , L & Tuononen , A J 2018 , ' A surface topography analysis of the curling stone curl mechanism ' Scientific Reports , vol 8 , no. 1 , 8123 , pp. 1-8 . DOI: 10.1038/s41598-018-26595-y en
dc.identifier.issn 2045-2322
dc.identifier.other PURE UUID: 04820219-84c6-441a-b56c-a9164ee90d0b
dc.identifier.other PURE ITEMURL: https://research.aalto.fi/en/publications/a-surface-topography-analysis-of-the-curling-stone-curl-mechanism(04820219-84c6-441a-b56c-a9164ee90d0b).html
dc.identifier.other PURE LINK: http://www.scopus.com/inward/record.url?scp=85047532806&partnerID=8YFLogxK
dc.identifier.other PURE FILEURL: https://research.aalto.fi/files/21763448/s41598_018_26595_y.pdf
dc.identifier.uri https://aaltodoc.aalto.fi/handle/123456789/31870
dc.description.abstract The curling motion of the curling stone on ice is well-known: if a small clockwise rotational velocity is imposed to the stone when it is released, in addition to the linear propagation velocity, the stone will curl to the right. A similar curl to the left is obtained by counter-clockwise rotation. This effect is widely used in the game to reach spots behind the already thrown stones, and the rotation also causes the stone to propagate in a more predictable fashion. Here, we report on novel experimental results which support one of the proposed theories to account for the curling motion of the stone, known as the "scratch-guiding theory". By directly scanning the ice surface with a white light interferometer before and after each slide, we observed cross-scratches caused by the leading and trailing parts of the circular contact band of the linearly moving and rotating stone. By analyzing these scratches and a typical curling stone trajectory, we show that during most of the slide, the transverse force responsible for the sideways displacement of the stone is linearly proportional to the angle between these cross-scratches. en
dc.format.extent 1-8
dc.format.mimetype application/pdf
dc.language.iso en en
dc.relation.ispartofseries Scientific Reports en
dc.relation.ispartofseries Volume 8, issue 1 en
dc.rights openAccess en
dc.subject.other General en
dc.subject.other 114 Physical sciences en
dc.title A surface topography analysis of the curling stone curl mechanism en
dc.type A1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä fi
dc.description.version Peer reviewed en
dc.contributor.department Engineering Design
dc.contributor.department Department of Applied Physics
dc.contributor.department Department of Mechanical Engineering
dc.subject.keyword General
dc.subject.keyword 114 Physical sciences
dc.identifier.urn URN:NBN:fi:aalto-201806183288
dc.identifier.doi 10.1038/s41598-018-26595-y
dc.type.version publishedVersion


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