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Behaviour of a sphere on a rough inclined plane
François-Xavier Riguidel, Remi Jullien, Gerald Ristow, Alex Hansen, Daniel Bideau
To cite this version:
François-Xavier Riguidel, Remi Jullien, Gerald Ristow, Alex Hansen, Daniel Bideau. Behaviour of a sphere on a rough inclined plane. Journal de Physique I, EDP Sciences, 1994, 4 (2), pp.261-272.
�10.1051/jp1:1994106�. �jpa-00246903�
Classification
Physics
AbstJ.acts46.30 64.60 68.22
Behaviour of
asphere
on arough inclined plane
François-Xavier Riguidel (~),
Remi Jullien(2),
Gerald H. Ristow(1),
Alex Hansen(')
and Daniel Bideau
(1)
(') Groupe
Matière Condensée et Matériaux(*),
Université de Rennes I,Campus
de Beaulieu, 35042 Rennes Cedex, France(2) Laboratoire des Sciences des Matériaux Vitreux (~*). Université de Montpellier II, Case 069, Place
Eugène
Bataillon, 34095 Montpellier Cedex 5, France(Received ii Jane J993, revised 7 September J993,
accepted
J2 October J993)Abstract. The tlifferent states of a bail on a rough indmed plane are analyzed from
experimental
results and numencal simulations. The conditions of static
equilibrium
are given. The control parameters are the inclination angle of the plane antl the surface roughness. Then, we propose a«phase
tliagram
» for the motion of the bail. These results are expectetl to be useful muntlerstantling
theongin
of thesegregatîon
effects on the surface of asandpile.
This paper is devoted to the
study
of the different regimes goveming the motion of oneparticle
on an indmed surface of controlledroughness (or smoothness).
Thegoal
of this workis to reach a better
understanding
of variousphenomena
occurrmg at the surface of aflowing granular
medium,especially segregation
:generally
if one observes the surface of agranular
medium(e.g,
a sandpile),
theIarger grains
are at the lower part, while the smallergrains
are at the top.Une of the most
important
mechanisms ofsegregatîon
is the surface flowil -3]
: the grainsnear the surface move on a
rough
surface which is theloyer below,
and theroughness
seenby
agrain depends
on its own sizecompared
to the size ofbumps
beneath it. Theforger
thegrain,
the less stable its
equilibrium position
when notmoving,
and thelonger
its « mean freepath
»L
along
theslope
when moving. Thisexplains why
onealways
finds theIargest grains
at the bottom ofpiles. Experiments
using a two-dimensional drum[4]
confirrn that surface flow is an important mechanism ofsegregation.
The
equilibrium
of asandpile
isgenerally
defined from theangle of
repose 0~, which is theslope
of apile
builtdynamically [5, 6]. However, starting
from thisangle,
such as inexperiments
onavalanches,
one can define the maximumangle ofstability 0~ [5] (or angle of
(~) URA CNRS n 804.
(.~*) URA CNRS n° II19.
JOLRNAL D~ PHYSIQUE T 4, N' 2 FEBRUARY <994
niaJ.gmctl stability [6])
as the maximumangle
for which thepile
is Table. Forexamp[e,
thisangle
may be measuredby tilting
thepile
until an avalanche occurs.However,
according
to the initial conditions and theangle
o between the inclinedplane
and the horizontal, the motion and theequilibrium
of aparticle
on arough
inclined surface i~ not asimple problem
to describe[7, 8].
Dursimplified
model pennits a formai andrelati~ely complete investigation
of thisproblem (roughness
and inclinationangle
are both controlparameters),
even if a directanalogy
with the surface of thesandpile
is non very strong. If one i~only
concemedby
the static behaviour, 1-e-by studying
the motion of the bail without any initial energy, we can define astability
threshold 0~. For ~o,,
the hall is stable,trapped
in awell at the surface.
Agam
with respect toequihbrium
ofpiles, 0,
is alocally
definedangle
ofmaximum
stability, depending mamly
on the geometry of the grains and that of the ~y;tem andto a fesser
degree
on the friction coefficient.If one gwes an initial kinetic energy to the hall, the
problem
becomes different. The hallmoves on the surface m a sort of directed random walk.
Starting
with an initial energy, themotion is first decelerated and, for small
enough
H, it stops. Forlarger
value~ of 0, the hall reache~ a constantspeed,
such as m the sedimentation of onepartide
submitted to Stokesdrag
force. When theangle
increases above a threshold value(,
the halljumps
on theplane,
and the scale of the motion iscompletely changed.
Thisregime
seems to be a transient one : the numefical simulations show thon after a verylong
lime, a new stationary regime i~ reached,with a constant
speed
and smalljumps.
The paper is
orgamzed
in thefollowing
manner in the first section we pre~ent the resu[t~ of theexperimenta[
and the numencal methods we used in thisstudy.
The second ~ectiondescribes our results concerning static behaviour, whereas we present in section three a
<~
phase diagram
» conceming the different kinds of behaviour observed in thedynarnic
ca~e.1.
Experimental
and numencal system.We want to model the surface of a «
sandpile
)>, but with control parameters which are theslope
of thepile,
and theroughness
of it~ surface. In order to do this, we use an inc[inedglas~
plane
P (one meterlong,
70 cm wide, and cmthick),
which can have a variableangle
i&.ith the horizontal. Theroughness
of theplane
is obtainedby ~ticking
smoothglas~ spheres
(of radius 1± 0.1 1) on contact paper fixed on theplane. Figure
shows a part of arough
~urfaceFig.
l Photograph of a pan of a rough surface obtainetl by sticking gla,~ beatl~ (tliametei 0.5 mm ona
plane.
The obtainetlpackmg
fraction is C 0.7.obtained
by
this method. The two-dimensional(2D) packing
ishomogeneous,
with apacking
fraction C 0.70-0.75. This is far from the usual
packing
fraction for dense disordered 2Dsystems (C 0.82) [9],
but seems togive
aroughness comparable
to that observed at the surface of apile.
Note that this 2Dpacking
is a disordered one. The radius of thespheres moving
down theplane
P isR,
and we define here the smoothness 4l of theplane
as the ratio Rli(the roughness
in thisparticular
casebeing
the ratioilR).
In one-dimensional
ID)
numericalsimulations,
we build an indmed row ofequal spheres,
whose distance between
neighbours
con berandomly
fixed between 2 r(touching spheres)
and2>.(1+ e):
seefigure
2. This mimics the disorder observed in 2Dexperiments
and simulations. The motion of one ball on this inclined row is studiedby
using moleculardynamics
simulationsdeveloped by
one of us[loi.
The hall can rotate and we considerdissipation
anddynamic
frictionduring
collisions. As anintegration scheme,
we use a third- orderpredictor-corrector algorithm [1Il.
Periodicboundary
conditions areimposed,
in such a way thatlong
distance motion con be studied.8
Fig. 2. ID motion of one ball on an inclined line. The roughness of the litre is createtl by placing balls
at rantlom or equally tlistanced positions. In the rantlom case, the distance between neighbours is
randomly
chosen between 2 r(touching
spheres) and 4 r.From the 2D numerical
point
of view, the ensemble ofequal
sized smallspheres
stuck on theplane
P is modeledusing
the randomsequential adsorption
model m two dimensions(RSA) just
below itsjamming
threshold, which is at apacking
fraction of C~ = 0,547[12].
In
figure
3 we show anexample
of such aconfiguration,
with apacking
fraction ofC
=
0.52,
built on a square ofedge length
L=
180 1, where r is the radius of the small
sphere,
withperiodic boundary
conditions at theedges
of the square. Thegeometrical properties
of such RSApacking
near thejamming
threshold have beenextensively
studied in the past[12].
We have
only reproduced
here thecomputations
that are necessary for the purpose of ourstudy.
We simulate the motion of alarger sphere by
assuming that italways
stays in contact with at least two smallerspheres dunng
its entiretrajectory (this
assumes that theangle
0should not be too
large
m order to prevent thesphere
fromjumping).
In this scheme, the detailsof the contact force between the moving
sphere
and the surfacespheres
areunimportant.
However, one can assume
sufficiently large
friction to make sure that therolhng sphere strictly
follows the
edges
of the Voronoipolygons,
mparticular
when it reaches a vertex where it has tochange
its direction quasiinstantaneously. Consequently,
mprojection
on P, thetrajectory
of the center of the
larger sphere
is made of successive segments which are alledges
ofVoronoi cells
[12]
of the RSAconfiguration
of the smallspheres. Figure
4 shows the Voronoi cellscorresponding
to theconfiguration
offigure
3.2. Static results :
stability
threshold.We studied 0~, the «
stability
» threshold first : it defines the limit ofstability
of a grain on thesurface,
anddepends
on the disorder of the 2Dpacking
stuck on theplane
and on thesmoothness 4l.
Fig. 3.
Fig.
4.Fig. 3. A typical RSA
configuration
obtainetl by numerical simulations with C= 0.52 (L
= 180 J
Fig. 4. Set of Voronoi ce[ls correspontling to the RSA
configuration
~hown m figure 3.Consider first the
problem
from a theoretical and numencal point of view in two dimensions.At each vertex, i-e- at each
point
i common to three Voronoi cells, where thelanger sphere
i~ incontact with three smaller
spheres
of centers A, B, C (seeFig. 5),
thelarge ~phere
has tochoo~e its way
according
to steepest descent rules. This can be determinedby ca[cu[ating,
atthe vertex point, the
respective slopes
of thepossible
furthertrajectofies
of thelarge
ballcenter. Let us calculate this
slope
for the motion in contact withspheres
A and B. We call x theunit vector
defimng
the steepest descent on P, y the unit vectordefining
thein-plane
horizontaldirection, and z
= x x y
perpendicular
to P. Inprojection
on P, the direction of motion i~defined
by
a unit vector u,perpendicular
to the segment AB. The unit vector t tangent, at thevertex point, the further
trajectory
of thelarge
bail center, is givenby
t = Cos qJu + sin ~Rz
z
~ t
tan~'zj
rll+©1
L ~ C
ti
Fig.
where the
angle
~R, indicated in
figure 5,
isgiven by
~~~ ~
N/(l
+~)2
r~ p~
~~
where h is the distance between the vertex point and the segment
AB,
and p is the radius of the circle which is circumscribedby
ABC. As a function of x, y and z, t is givenby
t = u~ Cos ~Rx + u~ cas ~Ry + sin ~Rz
(2)
and,
using
now the «laboratory
» set of unit vectors X, y and Z(X being
horizontal and Zvertical),
it isgiven by
t =
(u~
Cos ~R Cos à + sm ~R sin 0)
X + uy Cos ~Ry +(-
u~ Cos ~R sin à + sin~R Cos 0 Z
(3)
Consequently
theslope
a~ of t isgiven by
u~ cos ~R sin 0 + sin
~R Cos 0
a~ =
(4)
u~ cos ~R cos 0 + sin q~ sm 0Une can write
tx~ = tan
(&
à) (5)
with
tan &
= tan ~R
(6)
u~
8
might
bemterpreted
as a local thresholdangle.
If the actual inclination oislarger
than8,
therolhng sphere
can roll over AB.Using
equation(I)
and h=
iu,
where 1 is thealgebraic length
of iL(see Fig. 5),
one getstan &
~/~i
+~~
~.~
~~
~7)
If it is released at the vertex
point
without kinetic energy, theIarger sphere
is able to roll overAB if a~ SO, 1-e- if MS 0. At each vertex i, we define r~ as
being
the minimum oftan
Mi,
tan8~,
tan8~,
whereMi, 8~, 8~
are the threepossible angles
8(rolhng
over AB, BCor
CA).
If r~ is smaller than tan 0, alarge sphere
released at vertex without kinetic energy will rollnaturally
on thecouple
of smallspheres
whichcorrespond
to the minimumangle
8. If r~ isIarger
than tan 0, the vertex icorresponds
to a stableposition
of thelarge sphere.
Infigure 6,
we haverepresented
all thesteepest
descenttrajectories
starting from all the vertices(they
are the truetrajectories
for tan 0 m max~ r~. For smaller 0 values,only
some of thesetrajectories
areactually
used smce therolling
hall can betrapped
at somevertices). They
look like a network of rivers and tributaries with main avers closed on to themselves due topenodic boundary
conditions.In our numerical
calculations, starting
from an initial RSAconfiguration
we havedetermined the
r,'s corresponding
to all vertices of thecorresponding
Voronoi network. Thenwe have calculated the
quantity p(0 )
whichcorresponds
to the fraction of r~ values smaller than a given tan 0. When comparing with an experiment,p(0
also represents the fraction of balls which are able to move whenthey
are releasedanywhere
on P without initial kineticenergy. It is easy to define
stability
thresholds from these distributions : it is theangle
for whichp(0)
=
0.5,
as m the experiment. The results are given infigure
7. Une notices thatp(0
does net staff from p =0 for 0
=
0. This is due to the existence of some vertices which
Fig.
6. Ail ~teepe,t descent trajectories on Voronoi celledge~
for the RSA configuration ,hown in figure 3.° lt/r=2
~
. lt/r=4 Ù,4
,
° lt/r=16
0,2
0 10 20 30 40 50 60
8
Fig. 7. Curves giving p(0) as a function of à.
are «
naturally
» un~table, even for= 0 such vertices are located outside their
carre,ponding
ABC
triangles.
All the results that arereported
here have been obtained with L=
1801.
However, we have
performed
other calculation~ with different L values and we ha,,e checketl that for suchlarge
~ystems, the numefical results are quitemdependent
on the size as fat a~ we staysufficiently
close to thejamming
threshold.Experimentally,
H, is determmed on average as follows : at each experiment, 50 stee[spheres
(with diameters very well defined) areplaced
on the top of the (horizontal)plane,
each of thembeing
in stableequilibrium
m a « cavity » formedby
three smal[glass sphere~
incontact. This
explams
that is is notpossible
toexplore expenmentally
the non-stable situationsdescfibed
just
above : we must start with 50 halls in stableequflibrium.
From this initial situation, oisprogressively increased,
until onesphere
moves, and falls downalong
theplane,
and so on until all the 50spheres
are down, the expenment is done again.Finally, by
summingsix expenments (300
halls),
we have a(Gaussian)
distribution of limitequi[ibrium angles.
Figure
8gives
this distribution for4l=4,
and r=0.25 mm the mean value defines ô~. This distribution becomes wider antl wider when the smoothnessdecreases,
as shown infigure
9 which gwes the standard deviation of these distributions versus the smoothness4l,
in alog-log plot,
for r = 0.25 mm, r=
0.5 mm and r
= mm.
N ' r=lmm
° Î ° r=0,smm
é'oà
° r=0~25mm
. @
O
~
0 10 20 30 40 1 10 ioo
O
Fig.
8.Fig.
9.Fig.
8. Distribution of thestability angle
(~P = 4, antl r= 0.25 mm) as the resu[t of six elementary experiments (300 balls).
Fig.
9. Variations of the standartl-tleviation of the distribution of the static angle with the smoothness~P.
Figure
10 shows m alog-log plot
the variation of H~(normalized by
its value for 4l=
2)
versus the smoothness 4l.
Experimental
and numencal values are well fittedby
a unique curvecorresponding
to a power law H~ oz 4l~, with an effective exponent x =
0. 8. When companng
simulations with the expenments, the most
important approximation
appears to be the~~i
° Exp (r = 0,25 mm)
' Exp (r = 0,5 mm)
- . Exp(r=lmm)
C~
,
. simulations (C
= 0,52)
~°' ~~o
a
° simulations (C = 0,59)
~ o ,
ce
j
W ° o
à $
o .
o
lo~
1o° 1o~ o~
m
Fig.
10.Log-Log
plot of the variations of the stability thresholtl H~ (normahzetl by its value for ~fi 21 for tlifferent sizes of stuck balls (expenments) orpacking
fraction C on theplane
(2D numencalsimulations). All the results coalesce on a smgle curve well fittetl by a power law H~ cc ~P~~ with an exponent x = 0.8 ± 0.05.
replacement
of therough plane by
an RSAconfiguration.
Whendevising
therough plane,
thesticking
process iscertainly
morecomplicated
thon thesimple
rules of the RSA model. Inparticular
due to theunphysical
constraints of the RSA model, we are limited to aquite
lowconcentration
(lower
thon0.547)
whileexpefimental
concentration is of order of 0.7. We havealso
perforrned
similar calculationsusing
a more realistic RSA model. in which ~nmerestructuring
is allowed[1?].
With such a model one con reachhigher
densities of smallspheres
since thejamming
concentration islarger
(C m 0.61). The values obtained areonly slightly
srnaller than the previous ones, butcollapse
on the Sartre curve when normalizedby H,(2)
as can be seen infigure
10. Une can also believe thatfinding
0.8 and not is due to the fact that we are in the zone in which corrections to~caling
are important (and this zone growswhen the
packing
fraction increases), seeequation
(7).Another
interesting
result concerns the maximum value z~= tg H~, of the
T,'s,
to whichcorresponds H~
such that pi = I form
H~.
Ii can be calculatedexactly
at thejamming configuration
in the asymptotic hmit of aninfinitely large plane.
This shouldcorre~pond
to avertex with the
largest
p value, which is p=
2 r at
jamming,
and with aconfiguration
a; thatrepresented
infigure
11, i&.here thelarge sphere
should roll over a ~mal[sphere ju~t
in front of it. Thus=
2 r and one finds
T~ = tg
H~
= ~ j8), (4S -1)(4l + 3)
à
A
r r
x
c
Fig.
Il Sketch of aconfiguration
correspontling to 7= 7~.
Numerical simulations agree very well with this formula, but there are some differences with the experiment, whose results are
presented
infigure
12compared
to theoretical values. Alinear variation is also observed
expenmental[y,
but tanH~
is not zero at theongin
if weextrapolate
theexpenmental
results. This is due to the contribution of friction, andeventually
of attractive interactions between the ball and the stuck
glass spheres (capillary
forces..these forces ensure the
stability
of the hall on non-horizontalplane
(smal[ H) even for infinite smoothness.3.
Dynamical
behaviour,phase diagram.
In the above section, we have defined a
stability
threshold H~. which iscompletely
definedby
static conditions,mamly geometncal
ones. We are here concemed with aglobal analysis
of the differentdynamica[
regimes, and on itsdependence
on the geometry, i-e- on the smoothness of theplane.
In these expenments and in the lD numerica[ simulations, the bail is thrown on the3
R/r
' D
~im.ÎÎ
, BIC
° . Exn(r
m 0.25 mm)
° Exn(rmO.Smm)
. . Exp (rm mm)
~
a N1Im.olm. ~
o 50 ioo iso o ~ ~~ ~~ ~~
~'~~"
~
Fig.
12.Fig,
13.Fig. 12, Variations of tg H~ versus 2/
,~
accordingto
equation
(8). Thestraight
fine is the theoreticalprediction.
Fig. 13. ID phase tliagram obtainetl from numencal simulations (for s 0).
plane
with a small initial kînetic energy : we use adrawing
strawweakly
inclined with respectto the
plane
aslaunching
ramp. Thelength
necessary toforget
this initial kinetic energy is foundexperimentally
to be very smallcompared
to theplane length
(a fewcentimeters).
We have to compare here the static threshold H~ with thedynamic
threshold H~, which is defined in this section. But ourgoal
is to give aphase diagram
firstdescnbing
the differentdynamical
behaviour of the ball on a
rough
surface orhne,
with control parameters which are theangle
and the smoothness of the surface 4l. The ID
(numencal)
and 2Dphase diagram
are obtained.Figure
13 shows the 1Dphase diagram
for no disorder(e
=
0).
The contact conditions in thisexample
are thefollowing
: the coefficient of restitution in this simulation is 0.5. For small values of 4~(~ 0.8),
the behaviour of the ball isdependent
on its initialvelocity.
For 4~ ~ O.8, theplane
is divided in three parts,according
to the values of H. For small values of the inclinationangle (region A),
the motion is decelerated. Forangles roughly
between 5° and15°,
a constant
velocity
motion is observed(region B),
whereas forlarger angles (region D),
the ballvelocity
increasesleading
to motions in which steps arelarger
than the minimum onedefined
by
twoneighbounng
balls thusleading
tojumps.
The situation observed in 2D
experiments
is verycomparable. Figure
14gives
thephase
diagram
obtained, also with 4~ and as control parameters. In the A region, the motion is decelerated : the initial kinetic energy isquickly
lost. In the B region, a constantspeed
is observed, but the mean freepath (see
thequantitative
definitionbelow)
is smaller than the size of the table(2 m)
: the ball stops on theplane.
In the C region, thespeed
is constant, but themean free
path
islarger
than the tablelength.
In the D region,comparable
to itsequivalent
in the lDdiagram,
the bailjumps,
and the scale of the motion iscompletely changed.
We are
essentially
concerned with the constantspeed
regime. Acomplete analysis
of thedynamics
of thisproblem, including
statistical aspects, isgiven
elsewhere[7]. Briefly,
the motion is the result of a balance between the gravity force and a « viscous » force integrating«
microscopic
» collisions : so, the differentialequation descnbing
the average(1.e. neglecting fluctuations)
motion of the ball is identical to that of the Stokes sedimentation of asphere
m afluid. It is clear
expenmentally
that this stable motion issuddenly stopped
(notdecelerated) by
a
large
hole m the stuckpacking. According
to this observation, if one wants to descnbe the behaviour of the ballcompletely,
we must add to the constant motiondescription
aprobabihty
e~a~
fllr 2,8 ~"a~
D @~a~~
a~
a~
z ~~am~
c ea~
w a~~
© @~
m~~
A
~
0 4 a 2 16 20 40 60 80 100
8 1*
Fig.
14.Fig.
15.Fig. 14. 2D phase tliagram obtained from experiments.
Fig.
15.Semilog
plot of the cumulatetl distribution N(1
m 1* j of the stoppmg distance (1.e. number of spheres whose stoppmg distance Î is
larger
than a given valueÎ")
obtamed under the followmgconditions R
= mm, 1 = 0.25 mm,
= 4.7°, total number of spheres : 300.
for the ball to be
trapped
in a well. Thisprobabihty
is the sameeverywhere
on theplane
since itis
supposed
to behomogeneous,
and as a consequence, the distribution of the stoppmg distance1 (projection
of the distance coveredby
the ball beforestopping
on thelargest slope line)
forgiven
values of and 4l must beexponential.
This is what we observe, as shown infigure
15. which is asemilog plot
of the cumulated distribution of1.
The model descnbed
just
above allows us to make somequantitative predictions
concemmgthe
dynamical
parameters[7].
The meanvelocity
isgiven by
~~
~~(ÎÎ
~ ~~~where
f)
is the mean value of the(fluctuating)
Stokes constant, and m the mass of therolhng
ball. We find that
(f)
varies with 4l as 4~+~~~.Combining
the observed Stokes motion of the ball, and the use of extreme statistics toanalyse
the effects of traps on1,
we propose[7]
thefollowing expression
for the mean freepath
L on theplane,
defined as the averagecharacteristic value
of1
determined from distributions similar to that shown mfigure15 (L
~
(i)
L
(H,
4l =Lo
e~~~ =Lo e~'
~~~~~~~(10)
Table I
gives
different values of this mean freepath
L obtained from different values of and of the smoothness 4l. It shows inparticular
the very strongdependence
of L on theangle
and thesmoothness 4l: half a
degree
is sufficient tomultiply
Lby
5Starting
from the distributions of the stoppmg distance1,
we also define thedynamical
threshold H~ as
being
theangle
for which half of the balls have a stoppmg distancelarger
than theplane length. Figure16
shows the variations of H~(norrnahzed by
its value for 4l=
2)
»eisus the smoothness 4l, for three different values of r. The three curves coalesce m a well
defined power law H~ =
4l~",
where y=
1.55 ± 0.05.
Finally,
it is clear that H~ isalways
larger
than H~.Table I.
Dijfierent
valuesof
the meanfree path
obtainedf>.om dijfierent
valuesof
andof
the smaothness 4l,expi"essed
in cm. The tableÎength
is 200 cm.4l
(°)
4 5 6 8 lO31
1,3 29 95
1,7 136 ~ 200
2 45
~ 200
2,5 18 139
3 81
~ 200
3,5
10 ~2004 54
4,5 143
5 ~ 200
,~i
o
,o° o " ~*o,25mm
~
° r= O,5 mm
. * rm mm
m .
'
10'
~ o
4l
Fig. 16.
Log-log
plot givmg the variations of the dynamic threshold (normalized by its value for~P
= 2) ver.sus the smoothness for three values of r.
4. Conclusion.
Surface
phenomena
are of greatimportance
mrapid granular
flow. This paper is a contribution to basicunderstanding
of what are the relevant parameters in the motion ofpartiales
on thesurface of a «
sandpile
», with aparticular
attention to segregation effectsby
surface flow. Theresults obtained here outline the fact that on a
rough surface,
andespecially
on the surface of asandpile,
theequîhbrium
and the motion of onegrain
is verydependent
on its sizecompared
to the surfaceroughness.
The extremedependence
of the different thresholds and of the mean freepath
on the size of thepartiale
is at theorigin
of surfacesegregation
: even if our results are obtained for mdividualpartiales, they explain why
thelarge grains
are at the bottom of thepile (not trapped by roughness),
as observedby
numerical simulationsby
one of us[2].
Theseresults must be
completed by
a more accurateanalysis
of thedynamical
behaviour ofspheres
on a
rough
surface, and of collectiveeffects,
now m progress at Rennes.Acknowledgements.
We would like to
acknowledge
ourcolleagues
of thelaboratory,
and S. Roux for very useful discussions. This work wassupported
in partby
the CNRS ATP « MatériauxHétérogènes
»,and
by
theGroupement
de Recherche CNRS«
Physique
des MilieuxHétérogènes Complex-
es »
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