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Simulations of Dense Granular Flow: Dynamic Arches and Spin Organization
S. Luding, J. Duran, E. Clément, J. Rajchenbach
To cite this version:
S. Luding, J. Duran, E. Clément, J. Rajchenbach. Simulations of Dense Granular Flow: Dynamic Arches and Spin Organization. Journal de Physique I, EDP Sciences, 1996, 6 (6), pp.823-836.
�10.1051/jp1:1996244�. �jpa-00247217�
Simulations of Dense Granular Flow: Dynamic Arches and Spin Organization
S. Luding
(~>*),
J. Duran
(~),
E.C14ment (~),
J.Rajchenbach (~)
(~) Iustitut fur
Computerauweuduugeu
1,Pfaffeuwaldriug
27, 70569Stuttgart, Germany
(~) Laboratoired'Acoustique
etd'optique
de la Matibre Coudeus6e (**),,,Uuiversit6 Pierre et Marie
Curie,
4place
Jussieu, 75252 Paris Cedex 05, France(Received
lst December 1995, revised lstFebruary1996, accepted
26February 1996)
PACS.46.10.+z Mechanics of discrete systems PACS.05.60+w
Transport
processes:theory
PACS.47.20-kHydrodynamic stability
Abstract. We present a numerical model for a two dimensional
(2D) granular assembly, falling
in arectangular
container when the bottom is removed. We observe the occurrence of crackssplitting
the initialpile
intopieces,
like inexperiments.
Westudy
in detail various mech- anisms connected to the "discontinuousdecompaction"
of thisgranular
material. Inparticular,
we focus on the
history
of onesingle long
range crack, from itsorigin
at one sidewall,
until it breaks theassembly
into twopieces.
This event is correlated to an increase in the number ofcollisions,
I-e- strong pressure, and to a momentum waveoriginated by
oneparticle. Eventually,
strong friction reduces thefalling velocity
such that the crack may open below the slow,high
pressure
"dynamic
arch".Furthermore,
we report the presence oflarge, organized
structures of theparticles' angular
velocities in the dense parts of thegranulate
when the number of collisions islarge.
1. Introduction
The flow behavior of
granular
media inhoppers, pipes
or chutes has receivedincreasing
interestduring
the last years. For a reviewconcerning
thephysics
ofgranular materials,
seeii,
2] and references therein.The
complete dynamical description
ofgravity
driven flows is an openproblem
and forgeometries
likehoppers
or verticalpipes,
several basicphenomena,
are stillunexplained.
Inhoppers
intermittentclogging
due to vault effects(3], density
waves in the bulk (4] orI/f
noise of the outlet pressure, have been
reported
fromexperiments (5].
In a verticalpipe geometry,
numerical simulations on modelsystems
withperiodic boundary
conditions(6, ii
and also
analytical
studies (8] showdensity
waves. But sofar, experimental
evidence ofdensity
waves is
only
found in situations wherepneumatic effects,
I-e-gas-particle interactions,
areimportant (9].
In the
rapid
flowregime,
kinetic theories(lo,11]
describe the behavior of thesystem
in-troducing
thegranular temperature
as a measure of thevelocity
fluctuations. Inquasistatic
(*)
Author forcorrespondence (e-mail: lui@ical.uni-stuttgart.de) (**)
URA 800 CNRS©
Les(ditions
dePhysique
1996situations,
alsoarching
effects andparticle geometry get
to beimportant.
Under those con-ditions,
kinetic theories and also continuum soil mechanics do notcompletely
describe all thephenomena
observed. Thecomplicated particle-wall
andparticle-particle
interactions(12-14], possible
formation of stress chains in thegranulate
and also stress fluctuations(15,16]
undoubt-edly require
furtherexperimental,
theoretical and simulation work.Following
recent research on modelgranular systems (15-21]
we focus here on theproblem
of a 2D
pile
made up of ratherlarge spheres
enclosed in arectangular
container with trans- parent front and backwalls, separated by slightly
more than oneparticle
diameter. Recent observations ofapproximately V-shaped
microcracks invertically
vibratedsand-piles (I ii
werecomplemented by
recentexperiments
and simulations of the discontinuousdecompaction
of afalling sandpile (22].
Fromexperiments
Duran et al.(22]
find thefollowing
basic features: in a system withpolished
lateralswalls,
cracks areunlikely
to appearduring
thefall,
I.e. thepile
will accelerate
continuously,
with an acceleration valuedepending
on the aspect ratio of thepile
and on the friction with the walls.In a
system
with ratherpoorly polished
wallsla
surfaceroughness
of more than I /Lm insize),
cracks occur
frequently.
A crack in the lowerpart
of thepile
grows, whereas a crack in the upper part is unstable and willeventually
close. Theseexperimental findings
can be understood froma continuum
approach
based on adynamical adaptation
of Janssen's model(3,22]. Nevertheless,
not all of the discontinuous
phenomena,
such as the reasons for thecracks,
can beexplained by
such a continuum model. In
previous works,
numerical simulations were used toparallel
theexperiments
and toanalyze
thefalling pile
for different material'sparameters (22, 23]. Though
the simulations are
dynamic,
in contrast to anexperiment
which starts from a staticsituation,
a reasonable
phenomenological agreement
was found.Furthermore,
simulations were able to correlate the existence oflong
range cracks tostrong
local pressure on the walls. The increase inpressure was found to be about one order of
magnitude (22].
In this work we use the numericalmodel of references
(22-25]
andinvestigate
in detail how a crack occurs. Inparticular,
we follow onespecific
crack andtry
to extract thegeneric
features that could be relevant for amore involved
theoreticil description
of the behavior ofgranular
materials.We
briefly
discuss the simulation method in Section 2 andpresent
our results in Section 3 which consists of three mainparts: firstly,
we presentstick-slip
behavior and a localorganiza-
tion of the
spins
in Subsection 3.I.Secondly,
we describe in how far the number ofcollisions,
the kinetic energy and the pressure are connected in 3.2 andfinally
wepresent long
range or-ganization
and momentum waves in Subsection 3.3. We summarize and conclude in Section 4.2. The Simulation Method
Our simulation model is an event driven
(ED)
method(22,24-28]
based upon thefollowing
considerations:
particles undergo
aparabolic flight
in thegravitational
field until an eventoccurs. An event may be the collision of two
particles
or the collision of oneparticle
with a wall.Particles are hard
spheres
and interactinstantaneously; dissipation
and friction areonly
activeon contact. Thus we calculate the momentum
change using
a model that is consistent withexperimental
measurements(28].
From thechange
of momentum we compute theparticles'
velocities after a contact from the velocitiesjust
before contact. We account for energy loss in normaldirection,
as forexample
permanentdeformations, introducing
the coefficient of normalrestitution,
E. Theroughness
of surfaces and the connected energydissipation,
is describedby
the coefficient offriction,
/~, and the coefficient of maximumtangential
restitutionflo.
For interactions betweenparticles
and walls we use an index"w",
e.g. /~w. Due to the instantaneous contacts, I-e- the zero contacttime,
one may observe the so-called "inelasticcollapse"
in thecase of
strong dissipation.
For a discussion of this effect see McNamara andYoung (29]
andreferences therein.
Despite
thisproblem,
we use the hardsphere
ED simulations as onepossible approach,
since also thewidely
used softsphere
moleculardynamics (MD)
simulations may lead tocomplications
like the "detachment-effect"(30-32]
or the so-called "brake-failure" forrapid
flowalong rough
walls(33].
Recent simulations of the modelsystem,
described in thisstudy, using
an alternative simulationmethod,
the so called "contactdynamics" (CD) [14],
also lead to cracks
(34].
The CD method has a fixedtime-step,
in contrast to ED where thetime-step
is determinedby
the time of the next event.From the momentum conservation laws in linear and
angular direction,
from energy con-servation,
and from Coulomb's lawwe
get
thechange
of linear momentum ofparticle
I as a function of E, /~, and flo(25]
z~p
=
-m~~ji
+~)v(n) ~m~~ji
+fl)v(t), ji)
~ 7 ~
with the reduced mass m12
" mim2
f(mi
+m2).
Forparticle-wall interaction,
we set m2 " ccsuch that m12
= ml
In)
andit
indicate the normal andtangential components
of the relativevelocity
of the contactpoints
with v~ and w~
being
the
andangular velocities of article I just efore collision.
dz is
the of I and
the unit
vector
in ormal direction is here defindedn
= (ri -r2)f(ri
-fl
" mIn (flo>fill (3)
flo is the coefficient of maximum
tangential restitution,
-I < flo <I,
and accounts for energy conservation and for theelasticity
of the material(28]. fli
is determinedusing
Coulomb's law such that for solidspheres fli
" -Iii /2)/~(1+
E) cot ~ with the collisionangle ~/2
< ~ < ~(25]. Here,
wesimplifed
thetangential
contacts in the sense thatexclusively Coulomb-type interactions,
I-e-/hP(~)
is limitedby /~/hP("),
orsticking
contacts with the maximumtangential
resitution flo are allowed.
Sticking corresponds
thus to the case of lowtangential velocity
whilst the Coulomb casecorresponds
tosliding,
I.e. acomparatively large tangential velocity.
For adetailed discussion of the interaction model used see references
(24,
25,28].
3. Results
Since we are interested in the
falling
motion of acompact
array ofparticles,
we first prepare a convenient initial condition.Here,
we use N= 1562
particles
of diameter d= I mm in a box
of width L
=
20.2d,
and let them relax for a timetr
under elastic and smooth conditions until thedensity
and energyprofiles
do notchange
anylonger.
The choice of L isquite arbitrary,
however, we wanted to start with atriangular
lattice with a lattice constant ofd(I
+/h)
and /h to be small butlarger
than zero, I.e. /h= 0.01. We tested several
height
to width ratios S =H/L
of thesystem
and found e-g- the same behavior as inexperiments,
I-e- thelarger S,
thestronger
are the effects discussed in thefollowing.
The averagevelocity
of theresulting
initial condition is
=
fi
m o.05 mIs.
The kinetic energy connected to iscomparable
to the
potential
energy connected to the size of oneparticle.
Due to this rather low kinetic energy, the array ofparticles
isarranged
intriangular order, except
for a fewlayers
at thetop. Some tests with different values of lead to similar results as
long
as is not toolarge.
The
larger
@, the moreparticles belong
to the fluidizedpart
of thesystem
at thetop
and in the fluidizedpart
of thesystem
we can not observe cracks. For lower values of we observedan
increasing
number of events per unit time and thusincreasing computational
costs for the simulation. At t= 0 we remove the
bottom,
switch ondissipation
and friction and let thearray fall.
Performing
simulations with different initial conditions and different sets of material's pa-rameters,
we observe differences inposition
andshape
of the cracks.However,
theintensity
or the
probability
of the cracks seems todepend
on the material'sparameters
rather than on the initial conditions. The behavior of thesystem depends
on friction and ondissipation
as well: for weak friction we observeonly
randomcracks,
which would occur even in a dense hardsphere
gas without anyfriction, simply
due to random fluctuations and the internal pressure.With
increasing friction,
cracks may even span the wholesystem
and sometimes be correlatedto
slip planes. Furthermore,
we observe cracks to occur morefrequent
for lowerdissipation.
In
Figure
la we presenttypical snapshots
of anexperiment
and of a simulation at time t = 0.04 s. We observelong
range cracks fromboth, experiments
and simulations as well. For theexperiment
we use a container of widthL/d
= 24 with 103layers
of oxidized aluminumparticles.
The vertical 2D cell is made up of twoglass
windows for visualisation and of two lateral walls made ofplexiglass.
The gap between theglass
windows is a littlelarger
than the beaddiameter,
what leads to a small friction betweenparticles
andfront/back walls,
while the friction with the side walls may belarge.
Differentheights
and wall-materials were used and the results could be scaled with a characteristiclength (
=L/(2K/~w),
with thedimensionless
parameter
K which characterizes the conversion of vertical totangential
stresses and the coefficient of friction /~w. Thescaling
in theregime
before cracks occur leads to the valueK/~w
m 0.12. For a more detaileddescription
of theexperimental setup
and datasee reference
(22].
In the simulation ofFigure
la we have N= 1562 and the
parameters L/d
=20.2,
e =0.96,
Ew=
0.92,
/~ =0.5,
/~w =1.0,
andflo
= flow = 0.2. We varied the coefficients of friction in the intervals 0 < ~ < l and 0 < /tw < 10.Furthermore,
we varied the coefficients of restitution in the range 0.80 < E or Ep < 0.98.However,
the occurrence of cracks isquite independent
of the parametersused,
aslong
as the coefficients offriction,
/t and /tware
sufficiently large. Furthermore,
cracks occur faster forstronger dissipation
since ahighly dissipative
blockdissipates
the initial energy faster.For the above
parameters,
we find like inexperiments
alarge
number ofcracks,
over-lapping
andinterferring.
In the upper part ofboth, experiment
andsimulation,
we sometimesobserve cracks
only
on one side. In contrast toFigure
la we present inFigure
16 aspecific
simulation withonly
onestrong crack,
on which we focus in more detail, This crack sepa-rates the
system
into alarge
upper and a small lowerpart
and is best visible inFigure
16 att = 0.068 s. Here we use a reduced wall
friction,
I.e. /tw= /t =
0.5,
andstronger dissipation,
I-e- Ew
= E =
0.9,
while all otherparameters, including
the initialconfiguration,
are the sameas for
la).
In order to
distinguish consistently,
we will refer to the simulation withlarge
/tw as simulationla),
and to the simulation with small p~ as simulation16)
in thefollowing.
The
important
feature of the crack inFigure
16 is that it seems to be connected to onesingle Particle.
We indicate the verticalposition
ofparticle #371
with a small bar inFigure
16. The crack of simulation16)
is connected to an increase of the number of collisions perparticle,
indicatedby
thegreyscale
onFigure
16. Black or whitecorrespond
to zero or more thantwenty
collisionsduring
the last millisecondrespectively.
Note that the increase in the number of collisions is hereequivalent
to an increase in pressure.Already
at time t = 0.048 s,particle
#371 peforms
more collisions than the averageparticle.
The pressure aroundparticle #371
increases and at t= 0.056 s a
region
in which theparticles perform
alarge
number of collisionsj- 'm©
-~fi
(4÷÷)
~,j
(4÷9)
~
428i t/
(4÷÷j
()la' a)
~
~)
t = 0.048 s 0.056 s 0.064 s~
t=0.048
s0.052
s0.056
s0.060
s0.064
s0.068
sFig.
1.a) Snapshots
of atypical experiment (left)
and a simulation(right)
with n= 1562
particles,
at times t
= 0.06 s, in
a
pipe
of widthL/d
= 20.2. We used here Ew = 0.92, /~ = 0.5, yw = 1.0, and
flo = flow " 0.2.
b) Snapshots
from a simulation with almost the same parameters as inla),
but hereE =
0.90,
Ew = 0.90, and yw= 0.5. The
greyscale
indicates the number of collisions perparticle
per millisecond. Black and whitecorrespond
to no collision or more than ten collisionsrespectively. c)
Here
only
the selectedparticles
#369,#370,
#371, #390, #409, and #428from16)
areplotted
to illustrate their motion. The vertical line indicates theright
wall.spans the whole width of the container. We call such an array of
particles
underhigh
pressure"dynamic
arch". At t = o.o60 s the pressure decreases and alarge
crack opens belowparticle
#371.
At latertimes,
we observe new pressure fluctuations in the array. Inconclusion,
a crackseems to
begin
at onepoint,
I-e- oneparticle,
where the pressure increasesaccidentally.
Before we look in more detail at the behavior of
particle #371,
wepresent
forconvenience,
a
picture
of some selectedparticles
around#371
from16),
inFigure
lc.3.I. EViDENCE FOR STiCK-SLiP BEHAViOR. From
Figure
16 we evidenced that a crackmay
originate
from oneparticle only.
Now we are interested in thevelocity
of onespecific particle during
its fall.Following
the order of simulationsla)
and16)
wefirstly present
thecase of
large
wall frictionla)
andsecondly
the case of smaller wall friction16)
in thefollowing.
Remember that
particle #371
is theorigin
of onesingle
crack in simulation16),
while its behavior is similar to the behavior of manyothers,
close to theboundary,
in simulationla).
Due to
gravity,
theparticle
is accelerated downwards and after a collision with theright
wall it willpresumably
rotate counterclockwise.Therefore,
we compare the linearvelocity, Vz,
with the rotationalvelocity
of thesurface,
uJr. InFigure
2 weplot both,
the linear vertical and theangular velocity
ofparticle #371
as a function of time. The horizontal line indicateszero
velocity
and thediagonal
line indicates the free fallvelocity, -gt.
The full curvegives
the(negative)
linearvelocity
in verticaldirection, Vz,
while the rotationalvelocity
of thesurface,
uJr, is
given by
the dashed curve.Negative
cur valuescorrespond
to counterclockwise rotationand for Vz = uJr we have the contact
point
of theparticle
at rest relative to the wall. Theparticle adapts
rotational and linearvelocity,
or in otherwords,
the contactpoint
sticks. Thisevent occurs when the two curves merge. In
Figure
2a we observe a smallangular velocity
upto t m o.02 s when
particle #371
first sticks. Note that in this simulationla) #371
can not be identified as the initiator of one of the numerous cracks;however,
it sticks andslips
several times. An increase inangular velocity
goes ahead with a decrease of linearvelocity
due tomomentum conservation. At
larger
times we observe theangular velocity decreasing,
I-e- theparticle slips,
and short timeafter,
sticksagain.
Now we focus
on simulation
16)
and the behavior of theparticle,
from which the crack started.In
Figure
2b we observe a smallangular velocity
up to t m o.oso s. At t = o.055 s the velocitiesare
adapted
for some 0.005 s before theparticle slips again.
Since the pressure fluctuationsare visible in
Figure
16already
at t = 0.048 s, we conclude that pressure fluctuations in the bulk lead to asticking
of aparticle
surface on the wall. Thisparticle
is slowed down and thus willperform
more collisions with thoseparticles coming
fromabove,
what leads to an increase of pressure. An increase of pressureallows,
ingeneral,
astrong
Coulomb friction and thus asticking
of the contactpoint.
When pressuredecreases,
theparticle
surface does notlonger
stick on the wall.
Since the
sticking might
also occur betweenparticles,
we examine theangular velocity
of theparticles
in theneighborhood
of thesticking particle,
I.e. theparticles
to the upper left ofparticle #371.
InFigure
3 weplot
theangular
velocities ofparticles #371, #390, #409,
and
#428
for the simulationsla)
and(b).
We observe from bothfigures
as a response to friction, anauto-organization
of thespins
as also observed in lDexperiments
and simulations ofrotating
frictionalcylinders (12,13]. Spin
stands here for the direction ofangular velocity
of a
particle.
We see that the directneighbor
of#371
to the left andupwards,
I-e.#390,
rotates in the
opposite
direction of#371.
Thus a counterclockwise rotation ofparticle #371
leads to a clockwise rotation of
#390.
This is consistent with the idea of frictionreducing
the relative surface
velocity.
The nextparticle
to the upperleft,
I-e.#409,
isagain rotating counterclockwise, following
the same idea of frictionalcoupling.
InFigure
3a we observeonly
a weak
coupling
between#409
and#428,
whereas inFigure
3bparticle #428
is alsorotating
0.2
~~~
(( j
-gt
ji
~z~ -0.2
G
j
..-0.4 "....__
-0.6 "...,_
-0.8
0 0.02 0.04 0.06 0.08
t
is)
16)
~~ wr
Vz
-gt
~p 0
-,,---_,
~
, i
~/
~ -0.2
i~,
~ , ,,>,,
u ' ,---i,i,J
o , ii
z _04 '
>
-0.6 "..,_
-0.8
0 0.02 0.04 0.06 0.08
t
Is)
Fig.
2. Plot of theangular velocity,
uJr, and of the linear, verticalvelocity,
Vz, ofparticle #371
versus time. The simulations are the same as in
Figure
la and 16. The line -gtcorresponds
to afreely falling particle.
clockwise,
even when the absolute value of theangular velocity
is smaller. Thus we have notonly
astick-slip
behavior ofparticles
close to the sidewalls,
but also acoupling
of thespins
ofneighboring particles.
If thecoupling
isstrong enough,
we observe analternating,
butdecreasing angular velocity along
a line. We will return to this observation in Subsection 3.3.3.2. NiIMBER OF
CoLLisioNs,
KiNETiC ENERGY AND PRESSURE. Since the occurrenceof a crack
is,
ingeneral,
connected to alarge
number ofcollisions,
weplot
inFigure
4 the number of collisions perparticle
permillisecond, N~,
for simulationsla)
and16).
InFigure
4awe observe an increase in the number of
collisions,
which is related to the firststicking
event ofparticle #371. However, particles deep
in the arraypossibly perform
much morecollisions,
see#428
inFigure
4a.Obviously,
an increase inN~
for oneparticle
is connected to an increase inN~
for theneighbors.
InFigure
4b we find values ofN~ comparable
for directneighbors,
I.e.#371
and#390.
At t = 0.056 s we observe a drastic increase inN~
which also involves theparticles deeper
in the array, I.e.#409
and#428.
0.4
0.02
~ ~
lb) ~~~
04 #4°9
~_
f428
j~
0.2/~,,_,,
i
o
,~'
-0.2
-0.4
0 0.02 0.04 0.06 0.08
t
Is)
Fig.
3. Plot of theangular
velocities of theparticles
#371,#390, #409,
and#428
for thesame
simulations
as in
Figure
la and 16. Theseparticles
wereinitially arranged
on aline,
tilted clockwiseby
60degrees
from the horizontal, seeFigure
lc.In order to illustrate the reduced
falling velocity,
connected to alarge
number of collisions weplot
inFigure
5 theaveraged
kinetic energy K forparticles
betweenheights
z and z + dz(we
use here dz
= 0.002
m).
Weplot
K=
(I/N)L$ ~~) (disregarding
the mass of theparticles),
as a function of the
height,
z. Note that ~~ is thevelocity
of oneparticle
relative to thewalls,
and not relative to the center of mass of thefalling sandpile.
We observe different behavior for the simulationsla)
and16)
a ratherhomogeneous
deceleration of thepile
inla)
and one"dynamic
arch" connected to astrong
deceleration in16).
Forstrong
friction at the wallsla),
all
particles
in thesystem
are slowed down due tofrequent
collisions of theparticles
with the side walls and inside the bulk. For the times t =0.05, o.06,
and o.08 s weobserve,
from the bottom indicatedby
the left vertical line inFigure 5,
adecreasing
K withincreasing height
zup to z m 0.02 m, where the
slope
of K almost vanishes. InFigure
5b theparticles
arefalling
faster at the
beginning
until the firstdynamic
arch occurs at t m 0.056 s, seeFigure
16. Thehigh
pressure exerted on thewalls, together
with thetangential
friction at thewalls,
leads toa local
deceleration,
I.e. thedip
in the Kprofile
for t= o.06 s. This
dip
identifies adynamic
10000
(~)
# 371-
# 390 +
1000 # 409 D
x x # 428 x
SP
~x x
1
100 ~ x£
x x
Z ~*k
j~ x xx
ik
+ +
0 0.02 0.04 0.06 0.08
t
is)
10000(~)
# 371-
# 390 +
1000 # 409 D
~
# 428 x
1
~i
100~S
~ a
10
~
~ t+
~ +
a
~
~ ~
nn gg
0 0.02 0.04 0.06 0.08
t
Is)
Fig.
4.Log-lin plot
of the number ofcollisions,
Nc, per millisecond(ms)
as a function of simulation time, t. Plotted is Nc for the fourparticles
noted in thefigure.
The data are from the same simulationsas
already presented
inFigure
la and 16.arch of slow material which
temporarily
blocks the flow. Later intime,
theparticles
from above arrive at the slowerdynamic arch,
whichagain
leads togreat
pressure, alarge
number of collisions and thus to a further reduction of A'(see
the Kprofile
for t = o.08s).
In order to understand how the pressure in the bulk is connected to
N~
and K weplot
in
Figure
6 theparticle-particle
pressure, pp, inarbitrary
units as a function ofheight
for the simulationsla)
and16).
pp is here defined as the sum over the absolute normalpart
ofmomentum
change
pp(z, t)
=
L(/hPl")(, (4)
for each
particle
in alayer (z,z
+dz]
in a time intervalit,
tdt].
For thisplot
we usedz =
vsd (what corresponds
to aheight
of twoparticle layers)
and theintegration
time is here dt = o.oos s. For strong wall friction and lowdissipation la),
we observealready
at t = o.02 sa
quite strong
pressure with a maximum close to the bottom of thepile.
At t = o.05 s themaximum in pressure moved
upwards,
notonly
within thefalling pile
but also in coordinatez.
Furthermore,
the maximum is about one order ofmagnitude larger
than before.Later,
the0.8
~ ~ ~~~ t=0.02 s
t=0.05 s
o,6 t=0.06 s
~ t=0.08 s
~
0.5~
0.4E ..".-.._
~ 0.3
~,
".., 0.2
)"""~-,j,)"..._
0.1
"""~-£l-i=.===.=.."....=[)jj
0-0.04 -0.02 0 0.02 0.04 0.06 0.08
z
(m)
0.8
~ ~ ~~~ t=0.02 s
t=0.05 s
o,6 t=0.06 s
~ t=0.08 s
~
0.5~
0.4E .,.".,____
~ 0.3 "., _:."....-.--.,,__
0.2
"'~~~~~'~~~~~---__~
.,
0.I
'l~,,
0
-0.04 -0.02 0 0.02 0.04 0.06 0.08
z
(ml
Fig.
5. Plot of the kinitic energy K asa function of
height
z for different times for the same simulations asalready presented
inFigure
la and 16.pressure
peak
moved furtherupwards
and at t= 0.06 s
begins
to decrease until atlarger
times the array is dilute and pressure almost vanished. For weak wall friction16
we findonly
a weak pressure at time t = o.02 s until at time t = o.06 s a sudden increase of pressure, connected to the increase inN~
and the decrease inK,
appears. The occurrence of two pressurepeaks
of differentamplitude (small
pressure at the bottom andlarge
pressure at thetop)
is consistent with thepredictions
of Duran et al.(22],
which state that a small lowerpile
will be decelerated less than alarge
upperpile.
Thus the crack continuesopening.
3.3. LONG RANGE ROTATIONAL ORDER AND MOMENTUM WAVES. We have learned from
Figures
2 and 3that,
connected to alarge
number ofcollisions,
the direction of theangular velocity,
I.e. thespin
of theparticles,
may belocally arranged
in analternating
orderalong
lines oflarge
pressure. In order toproof
that this is notonly
a random event weplot
inFigure
7a onesnapshot
from simulationla)
and indicate clockwise and counterclockwise rotation with black and white circlesrespectively.
Weobserve,
at least in someparts
of thesystem,
thatspins
of the same direction arearranged along
lines. Thespins
of twoneighboring
lines have differentloco
(a)
tW.02s
(
100)-'/l~
t~°'05 s~
'
~"
t*0_06 8
~
' ' l,
i <' iv'
Jn
II I "~ '"'~~'m
li
~"" l '1
£
10'-
"""
c_
'
/
' '
".
i,/ '
' '
'
j
j /"'
'
-0.04 -0.02 0 0.02 0.04 0.06 0.08
z
Im)
iooo
16)
t=o o~ ~t=0.06 s
cz 100 ' t=0.08 s
I .'
" .,:".
~ 10 !
ib
",.j ,;
-0.04 -0.02 0 0.02 0.04 0.06 0.08
z
Im)
Fig.
6.Log-lin plot
of the pressure, pp, as a function ofheight
z for different times for the same simulations asalready presented
inFigure
la and 16.directions. The
elongation
of the orderedregions
may becomparable
to the horizontal size of thesystem. Note,
that lines ofequal spin
areperpendicular
to a line ofstrong
pressure, such that the order inFigure
7a indicates an arch like structure. For recentanalytic predictions
of theshape
of arches see(35].
In
Figure
7b weplot snapshots
from simulation16)
andplot
thechange
ofvelocity,
I-e-/h~~
=~~(t
+it) ~~(t)
and/h~z
=
~z(t
+it) ~z(t)
+ g it with bt=
lo~~
s.Comparing Figures
16 and 7b weidentify
thelarge
number ofcollisions, starting
fromparticle #371,
witha momentum wave
propagating
from#371
towards the left wall and alsodiagonally upwards.
When the momentum wave arrives at the left wall it is reflected and moves
mainly upwards.
We relate this to the fact that the material below the
dynamic
arch isfalling
faster than thedynamic arch,
such that not much momentumchange
takesplace
downwards. After several milliseconds the momentum wave is notlonger
limited to someparticles only,
but hasspread
and builds now an activeregion
withgreat
pressure, I.e. thedynamic
arch.Examining
the rotational order in simulation(b),
we observe that thespin
order is a con-sequence of the momentum wave. In our
model, strong coupling
is related to alarge
numbero
~~
t
=0.04
s'
j,~, >' ~ >~,, jj
~ ,) ,i ~ ~
,j,,
,[ [ l'j,')_ j => _'
~~
/,~
~'fi-
£'~ [ /
, t
/,
t =
0.053
s0.054
s0.055
s0.056
s0.057
sb)
Fig.
7.a) Snapshots
of the simulation fromFigure
la at time t = 0.04 s. The color indicates here the direction of theangular velocity,
I-e- black and whitecorrespond
to clockwise and counterclockwiserotation
respectively. b)
Snapshots from the simulation fromFigure
16 at different times. The lines indicate for eachparticle
thechange
invelocity
due to collisions within the last millisecond.of collisions and thus to a
large
pressure. This is due to thefact,
that informations about the state of theparticles
areexchanged only
on contact.Therefore,
lines ofequal spin
aremostly perpendicular
to the lines ofgreat
pressure, afinding
that is also discussed in reference(14].
4.
Summary
and ConclusionWe
presented
simulations of a 2Dgranular
modelmaterial, falling
inside a vertical container withparallel
walls. We observe fractures in the material which were described as a so-called"discontinuous
decompaction"
which is the result of many cracksbreaking
thegranular
assem-bly
intopieces
from the bottom to thetop.
The case ofhigh
friction andquite
lowdissipation (a)
is asystem
which shows the same behavior as also found in variousexperiments. Many
cracks occur and interfere. When we
investigate
anexemplary
situation with rather low friction andhigh dissipation (b)
we observe one isolated crack. We followed in detail the events which lead to this crack. Due to fluctuations of pressure(equivalent
to fluctuations in the number ofcollisions, N~),
someparticles
may transfer apart
of their linear momentum into rotationalmomentum. This
happens
when the surface of aparticle
with smallangular velocity
stickson the wall.
Sticking
means here that the velocites ofparticle
surface and wall surface areadapted.
The momentum wave,
starting
from such aparticle,
leads to aregion
oflarge
pressure, whichspans the width of the
system,
I-e- adynamic
arch. Due to thestrong
pressure, thedynamic
arch is slowed downby
friction with the walls. The materialcoming
from above hits thedynamic
arch such that adensity
and pressure wave,propagates upwards
inside thesystem.
Under conditions with
quite strong
wall friction and rather weakdissipation,
the fluctuations in thesystem
and also thecoupling
with the walls aregreater,
such that manyparticles
aresticking
on the walls. This leads to several pressure waves,interferring
with each other suchthat the
system
is slowed down morehomogeneously.
With the
dynamic
simulationsused,
we were able toreproduce
theexperimentally
observed discontinuousdecompaction (22]
and to propose anexplanation,
how the cracks occur. The openquestion remains,
if the situation discussed here is relevant for alltypes
ofexperiments
in restricted
geometries.
The features describedhere,
I-e- rotationalorder, stick-slip behavior,
and momentum waves are not
yet
observed inexperiments. Besides,
thephenomenon
ofstress fluctuations has been shown to be
important
forboth,
the behavior of static(16]
and ofquasistatic granular systems (15]. Furthermore,
the behavior of cracks inpolydisperse
or three dimensionalsystems
is still an openproblem.
Acknowledgments
We thank S. Roux for
interesting
discussions andgratefully acknowledge
thesupport
of theEuropean Community (Human Capital
andMobility)
and of thePROCOPE/APAPE
scientific collaboration program. The group is part of the FrenchGroupement
de Recherche sur la MatiAreHAtArogAne
etComplexe
of the CNRS and of a CEE network HCM.References
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