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PierreA. Gremaud 1

andJohnV.Matthews 1

DepartmentofMathematisandCenterfor ResearhinSientiComputation,

NorthCarolina StateUniversity,Raleigh,NC27695-8205,USA

Abstrat. Theproblemofdeterminingthesteadystateowofgranularmaterials

insilos undertheationof gravityis onsidered.Inthe ase ofaMohr-Coulomb

material, the stress equations orrespond to a system of hyperboli onservation

lawswithsouretermsandnonlinearboundaryonditions.Ahigherorder

Dison-tinuousGalerkinmethodisproposedandimplementedforthenumerialresolution

ofthoseequations.TheeÆienyoftheapproahisillustratedbytheomputation

ofthestresseldsinduedinsilos withsharphangesofthewallangle.

1 Introdution

Inthispaper,thesteadystateowofinompressiblegranularmaterials

un-der the ation of gravity is investigated. Of speial interest is the ase of

owsin silosandbins.Indeed,manufaturingindustriesroutinelystoreand

handle vast quantities of raw materials in granular form. The material is

usually retrieved through outlets at the bottom of the ontainers. Serious

diÆulties during the withdrawal proess are often observed. Those range

from deadzones ofmaterials stikingtheontainer's wallstoviolent

vibra-tionsthat anausethe ompleteollapseofthestruture. Inspiteoftheir

ommonness, those problems arepoorlyunderstood. It isproposed hereto

analyzenumeriallythestrutureandpropertiesoftheorrespondingows.

Thisworkis, totheauthors'knowledge,therstappliation ofahigher

or-dernumerialmethod{athirdorderDisontinuousGalerkinmethod{tothis

typeofappliations.

The two main physial assumptions, whih are disussed in Setion 2,

are that only established, steady state, ows are onsidered, and that the

materialis assumedto beeverywhereat yield.Mostof theexistingworkin

this eld deals with steady state owsin onial hoppers, i.e., when using

spherialoordinates,in domainssuhas

f(r;;');r>0;0<

w

;0'2g;

?

ThisresearhwassupportedbytheArmyResearhOÆe(ARO)throughgrants

DAAH04-95-1-0419andDAAH04-96-1-0097,bytheNationalSieneFoundation

(2)

whih orresponds to an innite, onverging hopper of half opening angle

w

. The attentiondevoted to this asestems from tworeasons. First, in a

greatnumberofappliations,theontainersareindeedaxisymmetri,ifnot

downrightpieewiseonial.Seond,asaonsequeneoftheinvarianeofthe

domain underthe salingtransformation(r;;') 7!(r;;') where >0,

similaritysolutions, theso-alled radialsolutions,an be onstruted.This

wasrst observed by Jenike [6℄, and hasplayed afundamental role in the

design ofindustrial hopperseversine[7℄, [11℄.Theradialsolutionsanbe

foundnumeriallybysolvingsystemsofordinarydierentialequations,more

preisely, boundary valueproblems. Theirbehavioris well doumented,see

e.g. [4℄, [8℄. Oneshould note, however, that the domain of appliability of

suhanapproahisquitelimited[5℄.Indeed,theveryimportantaseofthe

juntion between onial hoppers of dierent wall angles for instane, see

Figure1p.7,learlyannot betreatedundertheassumption ofradial

sym-metry.Further,eveniftheonsidereddomainshavetheneessarysymmetry

properties,ifandwhentheradialsolutionseetivelyorrespondto

approxi-mationsofwhatisobservedinpratieisnotlear.Thefullsystemofpartial

dierentialequationsdesribingtheproblemsathandhasthustobesolved.

Thisiswhereourontributionlies.

ThemodelispresentedinSetion2.Setion3isdevotedtothedesription

ofthenumerialmethod. Computationalresultsaredisussed andanalyzed

inSetion4.Finally,someonlusionsandremarksonfutureworkareoered

in Setion5.

2 The model

Theequationsgoverningthetimedependentowofgranularmaterialunder

gravityare derivedand analyzedin [12℄.Those are foundto belinearly

ill-posed in most ases of pratial interest. To the authors' knowledge, the

situation is not fully understood, mathematially orotherwise.In pratie,

stronglytime-dependentproblems areusually observedin onjuntionwith

funnel ows, i.e., ows for whih the motion essentially takes plae in the

entral part of the silo. This paperdeals exlusively with mass ows, i.e.,

ows for whih all the material is mobilized. In this ontext, established,

steadystateowsanbeobserved.

Thespatial domain is assumed to be axisymmetri,but notneessarily

rightonial. Thepartiles areassumed to haveno motionin the axial (or

') diretion.Even thoughthis assumptionmaybeounterintuitiveto uid

dynamiists,itisanestablishedexperimentalfatforgranularmaterials.The

stresstensortakestheform

T = 2

4 T

rr T

r 0

T

r T

0

0 0 T 3

5

(3)

Negletingtheinertialterms,onservationofmomentumyields

rT =g; (2)

inwhihisthedensity,takentobeonstant,andthevetorg isthe

ael-erationduetogravity.

Plasti deformation is assumed everywhere. Constitutive models based

on plastiity are onveniently expressed in terms of the prinipal stresses

i

;i = 1;2;3, i.e., the eigenvalues of the stress tensor T. If the prinipal

stressesare ordered

1

2

3

, thenthe Mohr-Coulombyield ondition

reads 1 3 =

1+sinÆ

1 sinÆ ;

where Æ is the angle of internal frition. This relation anbe derived from

thelawofslidingfrition[7℄,Chap.3.Thisonditionanbeexpressedinthe

originalstressvariables

(T rr T ) 2

+4T 2 r =sin 2 Æ(T rr +T ) 2 : (3)

The Haar-von Karman assumption an be invoked to evaluate the

ir-umferential stress T

''

. Indeed, the Mohr-Coulomb analysis merely states

1 T '' 3

.Foraxisymmetrionverginghoppers,theHaar-vonKarman

assumption states that T

''

is in fat the major prinipal stress. One an

writetheorrespondingequationsin termsoftwounknownsT

rr andT r T rr T r

=f(;;T

rr ;T r ) T r T

=g(;;T

rr ;T

r )

(4)

wheresomesimpliationsresultfromtheuseofthenewvariable = lnr;

wedonotbotherto renamethestressvariables. Therighthand sideterms

aregivenby

f(;;T

rr ;T r )= 3 s 2 T rr

+otT

r 3+s

2 T

+ge

os

g(;;T

rr ;T r )= 1+s 2

otT

rr +3T

r +

1 s

2

otT

ge

sin (5)

where we haveset s=sinÆ, and, forfuture referene, = p

1 s 2

=osÆ.

The equation of state, whih relates T

to the unknowns T

rr and T

r is

the yield ondition (3). It should be notied that (3) is the equation of a

one in the spae (T

rr ;T

r ;T

), whose entral line bisets the (T

rr ;T

)-plane.TheorrespondingrelationbetweenT

andtheunknownsistherefore

notaproperfuntional relation,but ratherassigns thedependent variables

(T

rr ;T

r

) tolie onamanifold: theyield surfae.Thesituation greatly

(4)

bearguedthatT

liesonthe\top"oftheyieldsurfae.Aordingly,by

solv-ing(3)forT

,theequationofstateompleting(4, 5)is

T

=h(T

rr ;T

r )

1+s 2

1 s 2

T

rr +2

s

s 2

(1 s 2

) 2

T 2

rr 1

1 s 2

T 2

r

: (6)

This orresponds to the so-alled passive state [7℄, [9℄, as opposed to the

ativestate whih is theother solution from (3), obtainedbyhangingthe

signinfrontoftheradialin(6);see x5.

Rewriting(4)as

U+

F(U)=G(;;U); (7)

with theobvious notation,oneanthen analyzetheeigenvalues

1;2 of the

JaobianF 0

. Afewalulationsleadto

1;2

=tanÆ 1

r

sT

rr T

r

sT

rr T

r

: (8)

A quikanalysis[3℄revealstheeigenvaluestobereal anddistint,provided

that onestays\inthe one",i.e.,j T

r

T

r r

j <tanÆ.Inother words,the steady

statestressequations(4,5,6)formastritlyhyperbolisystemofnonlinear

onservationlawswithsoureterms.Theradialandangularvariables and

anbethoughtofastime-likeandspae-likevariables,respetively.

Thesystemhastobeompletedwith\initial"andboundaryonditions.

The\initial" onditionused hereorrespondsto presribingthestresshigh

up in the hopper,say, on an\ =onstant" surfae,and solve down from

there.Severalargumentsanbeonsideredtojustifythefatthatthestress

information travels downward, see [3℄, [7℄, or [11℄ for more details. In the

alulationspresentedinthispaper,the\initial"onditionisomputedfrom

theradialstresseld;seex4fordetails.Finally,theboundaryonditionsare

givenbythelawofsliding frition.Atanypointonthewall,themagnitude

ofthetangentialstressjT

T

jisproportionalto themagnitudeofthenormal

stressjT

N j, i.e.,

jT

T

j=jT

N j;

where > 0is the oeÆient of wall frition. Ina purely radialgeometry,

theaboveboundaryonditionbeomes

T

r

=T

onthewalls (9)

witha\+"signononesideofthehopperanda\-"signontheother.Observe

that thoseonditionsarenonlinearintheunknownsT

rr ;T

r .

At this point, it is worth mentioning that the equations an in fat be

(5)

approahwasforinstanetakenin[8℄and[9℄.However,theuseof this

non-linear hange of variables has the unfortunate side eet of destroying the

onservationformoftheequations,losinginthiswaytheabilitytoompute

shoksin any reliableway. This prevents,for instane, theomputation of

stresses ourring at the juntion between onialhoppers of dierent wall

angles, oneofthemain goalsof this work.Further, asiswell known, many

purely numerialproblems also appear when solvingsystemsin

nononser-vationform.

3 The algorithm

For the sake of simpliity, we only desribethe algorithm in the ase of a

onial hopper. The method used is a formally third order Disontinuous

Galerkinsheme,see[2℄andtherefereneslistedtherein.

Let

0

= lnr

0

,wherer

0

isthevalueoftheradialvariablewestartfrom.

Let

w

>0bethehalf openingangle,andlet=

w

=N bethemeshsize,

N being the number of ells. In this axisymmetri setting, the problem is

spatiallyessentiallyone-dimensional,andthusnoeortshavebeenmadeto

adaptthemesh. Wedene

V =fv2L 1 (0; w ) 2 :vj Kj 2P k (K j ) 2

;j=1;:::;Ng;

whereK j =[ j 1 ; j

℄isthej-thell,with

j

=j,andP k

(K

j

)standsfor

thespae of thepolynomials ofdegreeat mostk in K

j

.We usek =2or3

below;seex4.AsemidisretizationonsistsoflookingforU

h

(;)2V, >

0 ,

suh that U

h ( 0 ;) = V (U( 0

;)), where U(

0

;) is an \initialondition",

seex4,

V

isaprojetionoperatorintoV, and

d d Z Kj U h

(;)v()d+

+ v( j 1=2 )H j 1=2 5 X l=1 ! l F(U h (; j;l )) d d v( j;l ) = 5 X l=1 ! l G(; j;l ;U h

(;))v(

j;l

); 8v2V;j=1;:::;N:

In the previous expression,

+

stands for the usual dierene operator,

+ U j =U j+1 U j

and the oeÆients!

l

and the nodes

j;l

, l=1;:::;5,

j = 1;:::;N stem from the use the lassial 5-point Gaussian quadrature

formula.Weusetheloal Lax-Friedrihsux

H j+1=2 = 1 2 F(U j+1=2

)+F(U + j+1=2 ) j+1=2 (U + j+1=2 U j+1=2 ) ; where j+1=2

isthemagnitudeofthelargesteigenvalueofaproperlyhosen

Roe average matrix A

j+1=2 ( dF ) U=U j+1=2

(6)

bakground. Themass matrix anbemade diagonal by hoosing the basis

funtions asLegendrepolynomialsovereahell[1℄.

The oeÆients of U

h

(;) an then be grouped in a vetor U(). The

unknownvetorU()satisesthefollowingsystemofODEs

d

d

U =F(U)+G(;U) (10)

where F(U) and G(;U) ome respetivelyfrom thedisretization of F(U)

and G(;;U) in (7). Note that we use below an unsplit approah. This

is justied rst by the fat that the soure term G(;U) is not sti and

seond,bytherealizationthatthedeliateinterplaybetweenG(;U)andthe

nonlinear boundary onditions would render the implementation of asplit

algorithmalotmoreinvolvedthanthepresentapproah.

Thedisretizationwith respet to involvesathird orderTVD

Runge-Kutta [13℄ ombined with a loal slope limitingproess. Let > 0be a

onstantinrementin andlet n

=

0

+n;thealgorithmreadsthenas

follows,see e.g.[2℄

{ SetU (0)

=(U

h (

0 ;));

{ Forn=0;:::;N 1,omputeU n+1

h :

1. setU (0)

=U n

h ;

2. fori=1;:::;3,omputetheintermediatestages

U (i)

=

0

i 1

X

j=0

ij U

(j)

+

ij (F(U

(j)

)+G( n

+d

j

;U

(j)

)) 1

A

;

3. setU n+1

h =U

(3)

.

The numerialparametersf

ij g,f

ij

gand fd

j

g,i =1;2;3,j =0;1;2are

respetivelydenedas

1

3=41=4

1=3 0 2=3 1

01=4

0 0 2=3 0

1

1=2

A thorough desription of the loal slope limiting operator , whih is

basedontheuse ofaorretedminmod funtion,anbe found,e.g.,in [2℄;

it isnotrepeatedhere.Notethat both andthe properimplementation

of the boundary onditions (9) requiretransformation to the harateristi

elds,see[3℄forimplementationdetailspertainingtothepresentappliation.

4 Computational results

(7)

θ

w

0

Γ

0

θ

w

w

-P

Q

Q

Θ

w

-

P

Fig.1.Geometrialsituation;left:transitiontoaatterwallangle,right:transition

toasteeperwallangle.Theradialstressisusedtogenerateaninitialonditionon

theurve

0

.Thedomainsofalulationareshaded.

AnypointP admitstworepresentations,namely,(R ;)and(r;),

orre-spondingto thenaturaloordinatesystemsfortheupperandlowerhopper

respetively. The transition is loated through the point Q, see again

Fig-ure 1,where Q=(R

0

;

w )= (r

0 ;

w

). For givenvalues of the material

parametersÆand,thenumerialapproahonsiststhenin

{ generating the radialstress eld T in the upper hopperf(R ;): R >

0;jj

w

g[4℄,[7℄;byonstrution,atapoint(R ;),theradialstress

eldisgivenbyRT();

{ interpolating the radial stress eld on the urve

0

= f(r;) : r =

r

0

;jj

w

g,leadingtoastresstensorS

0 ;

{ hangingtothenewoordinate systemthroughR T

( )S

0

R( ),

whereR()istherotationmatrixofangle;

{ solvingin thelowerhopperf(r;): 0<r <r

0

;0< <

w

gusing the

algorithmdesribedinx3.

Notiethatby(anti)symmetry,oneansolveinonehalfofthedomainonly,

thelawof slidingfrition (9) validon thewallsbeingreplaed bythe

sym-metryonditionT

r

=0ontheentralline.

Some omments are in order. First, the fat that the initial ondition

is generated from the radial stress eld impliitly assumes that this very

solutionissoughtandrealizedbytheproblemintheupperpartofthehopper.

Seond,italsotakesasgrantedthattheradialsolutionreahestheurve

0

unperturbedbythewallorner.Thislastpointislearlysatised,assuming

againadownwardpropagationoftheinformationforthestresses,inaseofa

transitiontoaatterhopper,i.e.,

w <

w

,seeFigure1,left.Ifthetransition

(8)

on theharateristi urvesreveals that the dierenein angles should not

betoolarge,namely

w

w

<artanj 1

max

j;

w ;

w >0;

where

max

isthelargesteigenvalueinmodulusofF 0

,see(8),evaluatedfor

the radial stress eld on the urvef(R

0

;) : jj

w

g.Third, the ase

w =

w

anbe used to hek that the algorithm eetively preservesthe

radial solution. The interation between the boundary onditions and the

foringterms rendersthis numeriallydeliate. Further,the radialsolution

itselfmaybeunstable[4℄.Thepresentapproahpreservestheradialsolution

withagreatdegreeofauray,see[3℄formoredetails.Finally,itshouldbe

noted that the above initial ondition is not onsistent with the boundary

ondition(9),unless

w =

w .

Inthealulationsbelow,theopeningangles

w and

w

arerespetively

takenas15 o

and 10 o

in arstexperiment,and as10 o

and12 o

,in aseond.

The material parameters orrespond to the ase of orn in a steel hopper.

The angle of internal frition Æ is 32:1 o

, while the angle of wall frition is

11:7 o

,in otherwords,thewallfritionis=tan11:7 o

.

Figure 2 orresponds to the ase of a transition to a steeper hopper,

whereas in Figure 3, the transition is to a shallower hopper. Some

predi-tionsaboutsuhtransitionsanbefoundintheliterature,seee.g.[7℄,x7.12.

Considerationsbasedon analogywithorresponding FluidDynamis

prob-lems and/or on the use of radial solutions have been advaned, prediting

smooth\rarefation"wavesfortransitionstosteeperhoppers,andshoksin

theaseoftransitionstowiderones.Wenoteherethatneitherofthosetypes

of arguments an be fully justied. The present results shed somelight on

thisproblem.

First,intheaseofatransitiontoasteeperhopper,theresultsreported

inFigure 2learlyshowthatthereisindeedformationofararefationwave.

Onean observe,however,thatafter thewavesgenerated onopposite sides

start to interat, they sharpen onsiderably and shoks appear. In Figure

2, both the P 1

and P 2

ases are reported. Although the P 2

results oera

slightlybetterresolution, theyalsosuerfromsmallosillationsthatanbe

observedaroundtheenterline. Thesmallosillationsstemfromnumerial

diÆultieslinkedtotheformoftheforingtermsthere,seetheottermin

(5),and thedeliateinterplaywiththelimitingproedure.Suhosillations

werenotobservedfortheP 1

ase.

Intheaseofatransitiontoashallowerdomain,theresultsofFigure 3

showthe immediateformationofshoks inthestresseld. Inthis ase,the

osillationsoftheP 2

alulationsaremorepronouned;weonlydisplaythe

(9)

0.6

0.65

0.7

0.75

0.8

0.85

0.9

0.95

−0.15

−0.1

−0.05

0

0.05

0.1

0.15

T

rr

/r, P

1

x

y

0.6

0.65

0.7

0.75

0.8

0.85

0.9

0.95

−0.15

−0.1

−0.05

0

0.05

0.1

0.15

T

r

θ

/r, P

1

x

y

0.6

0.65

0.7

0.75

0.8

0.85

0.9

0.95

−0.15

−0.1

−0.05

0

0.05

0.1

0.15

T

rr

/r, P

2

y

x

0.6

0.65

0.7

0.75

0.8

0.85

0.9

0.95

−0.15

−0.1

−0.05

0

0.05

0.1

0.15

T

r

θ

/r, P

2

y

x

Fig.2.Strutureofthestresseldinduedbyatransitionfromanopeningangle

of 15 o

to oneof 10 o

.Valuesof the parameters:Æ = 32:1 o

, =tan(11:7 o

) (orn,

steelwall).Firstrow,P 1

elements;seondrow,P 2

elements.

0.7

0.75

0.8

0.85

0.9

0.95

−0.2

−0.15

−0.1

−0.05

0

0.05

0.1

0.15

0.2

T

rr

/r, P

1

y

x

0.7

0.75

0.8

0.85

0.9

0.95

−0.2

−0.15

−0.1

−0.05

0

0.05

0.1

0.15

0.2

T

r

θ

/r, P

1

y

x

Fig.3.Strutureofthestresseldinduedbyatransitionfromanopeningangle

of 10 o

to oneof 12 o

.Valuesof the parameters:Æ = 32:1 o

, =tan(11:7 o

) (orn,

steelwall).P 1

(10)

5 Conluding remarks

We have presented a numerial study of stress elds indued by the

dis-hargeof granularmaterialsinhoppers.Thestress equationsorrespondto

asystemof hyperbolionservationlawswithseveral nonstandardfeatures.

A higherorder DisontinuousGalerkin method hasbeenimplemented. The

orrespondingnumerialresultspartiallyonrmseveral\eduatedguesses"

thathadbeenmadeaboutthestresseldstrutureinduedbyhangesinthe

wallangle.Amoreompletepitureoftheowshouldinvolvetheresolution

oftheveloityequations,whihwillbeoveredin futurepubliations.

Aknowledgments

TheauthorswouldliketothankDavidShaeerandMihaelShearerfor

manyhelpfuldisussions.

Referenes

1. Cokburn,B.,Lin,S.Y.,Shu,C.W.:TVBRunge-Kuttaloalprojetion

dison-tinuousGalerkinniteelementmethodforonservationlawsIII:onedimensional

systems.J.Comput.Phys.84(1989)90{113

2. Cokburn,B.,Shu,C.W.:TheRunge-KuttadisontinuousGalerkinmethodfor

onservationlaws V: multidimensionalsystems.J. Comput. Phys. 141(1998)

199{224

3. Gremaud,P.A.,Matthews,J.V.:Ontheomputationofhopperows.In

prepa-ration.

4. Gremaud, P.A.,Matthews, J.V.,Shearer, M.: Similarity solutionsfor granular

owsinhoppers.ProeedingsoftheSIAM/AMSConfereneonNonlinearPDEs,

DynamisandContinuumPhysis,J.Bona,K.Saxton,R.Saxton,Eds.,(1998),

AMSContemporaryMathematisSeries,tobepublished.

5. Gremaud, P.A., Shaeer, D., Shearer, M.: Numerial determination of ow

orretiveinsertsforgranularmaterialsinonialhoppers.SubmittedtoInt.J.

NonlinearMeh.

6. Jenike, A.: Gravity ows of bulksolids. Bulletin No. 108, vol. 52, Utah Eng.

Expt.Station,UniversityofUtah,SaltLakeCity(1961)

7. Nedderman,R.M.: Statiandkinematiofgranularmaterials.Cambridge

Uni-versityPress(1992).

8. Pitman, E.B.: The stability of granular ow in onverging hoppers. SIAM J.

Appl.Math. 48(1988)1033{1052

9. RaviPrakash,J.,KesavaRao,K.:Steadyompressibleowofohesionless

gran-ularmaterialsthroughawedge-shapedbunker.J.FluidMeh.225(1991)21{80

10. Roe, P.L.: Approximate Riemann solvers, parameter vetors, and dierene

shemes.J.Comp.Phys.43(1981)357{372

11. Royal,A.T.:Privateommuniation.Jenike&Johanson,In.(1998).

12. Shaeer,D.G.:Instabilityintheevolutionequationsdesribinginompressible

granularow.J.Di.Eq.66(1987)19{50.

13. Shu, C.W., Osher, S.: EÆient implementation of essentially non-osillatory

References

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