Rubber snow interface and friction
dc.contributor.advisor
Blackford, Jane
en
dc.contributor.advisor
Koutsos, Vasileios
en
dc.contributor.author
Ella, Sam
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dc.contributor.sponsor
Michelin
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dc.date.accessioned
2016-11-22T14:13:04Z
dc.date.available
2016-11-22T14:13:04Z
dc.date.issued
2014-06-30
dc.description.abstract
Tyres are used in everyday life for a variety of practical and recreational tasks.
Frictional behaviour of tyres on any surface is important for vehicle safety and
control; this behaviour becomes more important when that surface is snow. The
interaction of rubber and a snow surface is complex and a deeper understanding of
both is needed in order to help develop better tyres.
Outdoor full scale tyre test results were compared to results from indoor laboratory
tests using a linear tribometer and a surface of compacted artificial snow; these were
in excellent correlation allowing a systematic and comprehensive study of rubber
friction on snow to be conducted in the laboratory. Rubber samples of varied rubber
compositions and geometries were used to gain an understanding of friction on snow.
Samples with varying glass transition temperature (Tg), dynamic rigidity (G*) and
Payne effect (dependence of the dynamic moduli on the amplitude of the applied
strain) were investigated along with samples with and without sipes. The rubber
friction coefficient (μ) was measured as a function of velocity and temperature. The
siped samples exhibited a higher μ than those without sipes. FE simulations, rubber
friction tests for varying contact pressures and steel blade force tests were performed
to evaluate contributions from ‘surface’ friction and ploughing separately. The
increased μ was attributed to the ploughing force from the front edges of the ‘subblocks’
created by the sipes. Although it is well known in the industry that siped
tyres grip well, this is the first time it has been explained how sipes grip effectively
through a combination of ploughing and rubber snow interaction.
A comprehensive study of varying rubber properties (Tg, G* and Payne effect) was
conducted to better understand their impact on snow friction. The findings were
evaluated using the WLF shift factor to account for the running frequency of the
rubber from the snow surface roughness. G* was found to be the dominant parameter
for rubber μ when considering running frequency. Increased μ values were exhibited
by rubbers with a lower G*. The decreased G* makes the rubber more compliant,
thus increasing the contact area between the rubber and the snow, in turn increasing
μ.
A better knowledge of the surface roughness of snow will aid the understanding of
the interaction between rubber and snow for tyres. A method was developed to
characterise the artificial snow surface utilising sectioning and imaging of chemically
stabilised snow samples. From images of the snow surface before friction testing the
average indentor size can be found, this is used to analyse the running frequency of
the rubber. Qualitatively comparing the surfaces before and after rubber friction
testing shows a decrease in surface profile aggressivity after a test; this is attributed
to melting of the snow from frictional heating and snow grain fracture.
Friction tests were conducted to directly compare rubber friction on snow and ice
using round edged samples. Again it was found that the rubber with the decreased G*
exhibited higher friction; this was seen on both snow and ice confirming G* as the
dominant rubber property for both surfaces, regardless of the surface roughness
change. It was found that at low temperatures ice had a higher μ than snow, while at
high temperatures snow exhibited a higher μ than ice. It is hypothesised that this
intriguing switch is due to the surface roughness change leading to differing contact
areas both with and without melt water. This switch is not seen when a simple heat
transfer model is used, confirming the effect as a surface roughness change. The use
of a modified Hertz model shows that indentation is the dominant mechanism at low
velocities on snow. It is hypothesised that at high velocities melt water dominates on
both snow and ice while adhesion may have a more significant role on ice at low
velocities. These findings provide knowledge that can be used in the design of tyres
for snow and ice in the future.
en
dc.identifier.uri
http://hdl.handle.net/1842/17941
dc.language.iso
en
dc.publisher
The University of Edinburgh
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dc.relation.hasversion
Ella S, Formagne P-Y, Koutsos V and Blackford JR 2013 Investigation of rubber friction on snow for tyres Tribology International vol 59 pp. 292-301
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dc.rights.embargodate
2100-12-31
dc.subject
snow
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dc.subject
rubber
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dc.subject
friction
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dc.subject
interface
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dc.subject
roughness
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dc.subject
temperature change
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dc.title
Rubber snow interface and friction
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dc.type
Thesis or Dissertation
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dc.type.qualificationlevel
Doctoral
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dc.type.qualificationname
PhD Doctor of Philosophy
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dcterms.accessRights
Restricted Access
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