where s isthestresstensorand f(q,x,t)isaforcedensity(perunitvolume squared)thataneighboringpoint q exertson x.Thisforcedensityis determinedbythedeformationaccordingtothematerialmodel.Itis alwaysrequiredasaconsequenceofNewton’slawsthat
forall x, q, t.Theregionofintegrationin Eq.(1.1) isthe family of x,which isaneighborhoodwhoseradius d > 0iscalledthe horizon (Fig.1.1).
Thehorizonisacutoffdistanceforforceinteractions.
Using Eq.(1.1),theperidynamicequationofmotionisasfollows:
where r isthemassdensity, y isthedeformationmap,and b isthe externalbodyforcedensityfield.Theattributeofthetheorythatallows interactionsbetweenpointssuchas x and q directlyacrossafinitedistanceissometimescalled strongnonlocality.
Inintroducingperidynamics,thebasic Eq.(1.3) isusuallypresentedas anassumptionthatiselaboratedupontoshowthatithasdesirable properties,suchasbeingabletosustaingrowingcracks,andnotviolating anylawsofphysics(Silling,2000).Thisleavessomepeoplewondering, “Wheredoesthiscomefrom?”Inparticular,thestronglynonlocalnature of Eq.(1.3) isperceivedaslackingmotivation.Withthisinmind,Ihope
forall k, [,and t.Itisalsoassumedthatthereisacutoffdistance d forthe atomicinteractionssuchthat Fk[ ¼ 0if jx[ xk j > d.
Additionally,particle k issubjecttoaprescribedexternalforce Bk(t).For any x˛R3,defineasmoothingfunction U(x, $)suchthatthefollowing normalizationholds:
foranypoint p.Itisconvenienttoassumethatatany x, U(x, $)vanishes outsideaneighborhoodofradius R,where R isapositivenumber.Define thesmoothedmassdensityandbodyforcedensityfieldsby
Definethesmootheddisplacementfieldby
Nowweinvestigatetheevolutionequationfor u.Theparticlesobey Newton’ssecondlaw, Mk € uk ðtÞ¼ X [ Fk[ ðtÞþ Bt ðtÞ.(1.8)
Differentiating Eq.(1.7) twicewithrespecttotimeyields rðxÞuðx; tÞ¼ X k Uðx; xk ÞMk uk ðtÞ (1.9)
From Eqs.(1.6),(1.8),and(1.9),
rðxÞ € uðx; tÞ¼ X k Uðx; xk Þ"X [ Fk[ ðtÞþ Bk ðtÞ# ¼ X k X [ Uðx; xk ÞFk[ ðtÞþ bðx; tÞ (1.10)
From Eqs.(1.5)and(1.10),
rðxÞuðx; tÞ¼ X k X [ Uðx; xk ÞFk[ ðtÞ Z Uðq; x[ Þdq þ bðx; tÞ (1.11)
Eq.(1.11) canberewrittenasfollows:
rðxÞuðx; tÞ¼ Z fðq; x; tÞdq þ bðx; tÞ (1.12)
where
and b isgivenby Eq.(1.6).Itiseasilyshownfrom Eqs.(1.4)and(1.13) that f hastheantisymmetry Eq.(1.2).Thevectordefinedby x ¼ q x (1.14) iscalleda bond.(Whentalkingaboutbonds,itisalwaysassumedthat x s 0,withoutexplicitlystatingthis.)Thefunction f iscalledthe pairwise bondforcedensity andhasdimensionsofforce/volume2.From Eq.(1.13), thepoints x and q interactonlyif
Thelength d isthehorizonforthecontinuummodel(Fig.1.1).
Insummary,wedefinedaweightingfunction U andusedittodefine smoothedfields r, b,and u.Withthesedefinitions,andNewton’ssecond lawappliedtotheparticles,thesmootheddisplacementfieldwasfound toobeytheperidynamicequationofmotion Eq.(1.12).Theperidynamic bondforcesthatappearinthisequationofmotionaredefinedby Eq. (1.13).Conceptually,theequationofmotionis,andshouldbe,nonlocal becausechangingthedisplacementofasingleparticle k directlyaffects thesmootheddisplacementsatallthepoints x whosesmoothingfunction U(x, $)havenonzerovaluesat xk.Amorecompletederivationofthe peridynamicequationswasobtainedfromstatisticalmechanicsby LehoucqandSears(2011).
Thedefinitionofthepairwisebondforcedensity Eq.(1.13) isnotvery practicalasamaterialmodelbecauseitdoesnotdirectlyrelatethevalues of u near x tothebondforces f.Morepracticalmethodsofdetermining f arediscussedin Section3.
3.Materialmodels
Thepurposeofamaterialmodelinperidynamicsistodeterminethe valuesofthepairwisebondforcedensity f(q,x,t)intermsofthesmoothed displacementsinthevicinityof x and q andanyotherphysicallyrelevant fieldssuchastemperature.(Theword“smoothed”willbeomittedfrom nowon,sincewearenolongerconcernedwiththeunderlyingatomic system.)Itisassumedthatthereisahorizon d,suchthat
Thestrainenergydensitygivenby (1.22) hasthesamemeaningasin thelocaltheory,sinceitrepresentsthepotentialenergyperunitvolume thatisstoredat x duetodeformationofthenearbymaterial.Ifthematerialisisotropicaswellaslinearmicroelastic,thisinterpretationprovidesaneasywaytocalibrate c(x)ifthegeneralformofthedependenceof c onbondlengthisgiven.Foranisotropicmaterial, c(x)dependsonlyon thebondlength, x ¼ |x|.Byrequiringtheperidynamicstrainenergy densitygivenby (1.22) toequalitsvalueinthelocaltheoryforanisotropic expansion,itiseasilyshownthat c isrelatedtothebulkmodulus k bythe followingexpression(SillingandAskari,2005):
Thus,withthesimplifyingassumption Eq.(1.24),ifthehorizon d is given,theonlyparameterinthelinearmicroelasticmaterialmodelis easilycomputedfromthebulkmodulus.
Thelinearmicroelasticisanexampleof bond-based peridynamicmaterialmodels.Thisclassofmaterialmodelshasthepropertythatthe pairwiseforcedensityinthebond x ¼ q x isfullydeterminedbythe deformationofthatparticularbond,anddoesnotdependonwhathappensinotherbonds.
Bond-basedmaterialshavetheadvantageofbeingsimpletounderstandandcalibrate.Theyallowforgeometricnonlinearity,becausethe bondsrotatealongwiththebondsastheydeform.Theyconserveangular momentum,becauseregardlessofthedeformation,eachpairwisebond forceexertszeromomentontheendpointsofthebond.Bond-based materialmodelscanincludematerialnonlinearity,aswellasgeometric nonlinearity,byusingafunction b f in Eq.(1.19) thatincludesnonlinear dependenceonthebondstrain.
where m isabinary-valuedfunctionthatstartsat1anddropsto0accordingtosomeprescribeddamagecriterion.Thesimplestsuchcriterion breaksabondwhenitsstrainexceedssomepredefinedvalue s0:
where H istheHeavisidestepfunctionand tbreak istheearliesttimeat which s(x,t) s0.Thelinearmicroelasticmaterialusing Eq.(1.24) and equippedwiththebondbreakagecriteriongivenby Eqs.(1.26)and(1.27) iscalledthe prototypemicroelasticbrittle (PMB)materialmodel.
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