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Joe GODDARD Department of Mechanical and Aerospace ...

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ColloqueTraffic <strong>and</strong> Granular Flows 07Paris-Sud University, Orsay<strong>Joe</strong> Goddard<strong>Department</strong> <strong>of</strong> <strong>Mechanical</strong>& <strong>Aerospace</strong> EngineeringUniversity <strong>of</strong> California,San Diego (La Jolla)From Granular NetworkstoGraded Continua


Outline• The multipolar continuum as a model for granular medawith “length-scale” effects• A recently proposed homogenization scheme based ongraph theoretical ideas <strong>and</strong> energy principles*• A toy model <strong>of</strong> particulate flow, with conclusions <strong>and</strong>open questions• See “From Granular Matter to Generalized Continuum”, in Mathematical Models <strong>of</strong>Granular Matter, P. Mariano et al. (eds), Springer Lecture Notes in Mathematics, toappear 2007. (Qualified research students are invited to attend a school“Structures <strong>of</strong> the mechanics <strong>of</strong> complex bodies” in the Centro di Giorgio,University <strong>of</strong> Pisa, Italy, October 1-7, 2007.)


Multipolar effects - Why should we care?• Granular media are susceptible to a number<strong>of</strong> material instabilities. In quasi-staticmotions, these lead to “strain localization”,usually in the form <strong>of</strong> “shear b<strong>and</strong>s” <strong>of</strong> theorder <strong>of</strong> 10 grain diameters thick, in bothexperiment <strong>and</strong> numerical simulations.• Experimental observations <strong>and</strong> computersimulations suggest that the particle rotationsin such regions are different from the globalrotation (or vorticity), sometimes interpretedas “Cosserat” effects.• Some type <strong>of</strong> “enriched continuum” model isnecessary to regularize simple continuum models,numerically if not physically. The associatedgradient effects may influence material instability(Aifantis, Vardoulakis <strong>and</strong> coworkers, 80’s +).• Same ideas may apply to continuum models <strong>of</strong>traffic flow.


<strong>Mechanical</strong> Networks (& Delaunay Graphs)Examples:Materialrubberdry foamgranular mediumElementspolymer chainsPlateau bordersparticle contactsNodesentanglementsborder junctionsparticle centroids


From grains to branches<strong>and</strong> simple continuummodelal_


Granular contact (Satake) graphs


From weightedgraph to continuum


From simple to multipolarcontinuum(Toupin, Mindlin, Green & Rivlin,“Graded Continuum”)(Cosserat, Green & Rivlin, Eringen“Micromorphic” Continuum)


Extrinsic granularmodesSubscripts “k ” referto contacts or edges (ij) .


Homogenization (extrinsic modes)


LSE in GAM** Proposed by M. Rosenblatt some 30 years ago for spline smoothing <strong>and</strong> later dubbed “GAM”(Wood, S. N. J. Am. Stat. Assoc. 99, 467, 2004).


Possible alternative


Toy “micr<strong>of</strong>luidics” problem** Future calculation will involve MD data <strong>of</strong> J. Koplik for flow <strong>of</strong> Lennard -Jones fluid in a slot. Similar data for granular mechanics would be welcome.


Homogenization with latest LSE+GAMLSE fit to noisy quadraticu = Δv vs. y (/particle diam.)with 5th-deg. polynomialLSE+GAM fit• Note that GAM transfers energy from quadratic to linear terms


Conclusions <strong>and</strong> Questions• One can associate a graded multipolar continuum to theextrinsic degrees <strong>of</strong> freedom represented by granular centroids.• Although not discussed in detail above, this modifies the st<strong>and</strong>arddefinition <strong>of</strong> (Cauchy) stress, since lower-order stresses areaffected by higher-order terms.• A proper energy-based homogenization still leaves some freedom<strong>of</strong> choice in least squares estimates (LSE) with generalized additivemodel (GAM) to avoid overfitting. This is a basic physical problem<strong>of</strong> distinguishing fluctuations from higher-gradient effects. Is therethere some physically preferred resolution?• Simulation data <strong>and</strong> new ideas welcome.Thanks for your attention!

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