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Eurich *\nInstitut fu\u00a8r Theoretische Physik, Universita \u00a8t Bremen, Otto-Hahn-Allee 1, D-28334 Bremen, Germany\nJ. Michael Herrmann\nMax-Planck-Institut fu \u00a8r Stro\u00a8mungsforschung, Bunsenstrasse 10, D-37073 Go \u00a8ttingen, Germany\nUdo A. Ernst\nInstitut fu\u00a8r Theoretische Physik, Universita \u00a8t Bremen, Otto-Hahn-Allee 1, D-28334 Bremen, Germany\n~Received 14 September 2000; published 31 December 2002 !\nWe study the avalanche dynamics of a system of globally coupled threshold elements receiving random\ninput. The model belongs to the same universality class as the random-neighbor version of the Olami-Feder-Christensen stick-slip model. A closed expression for avalanche size distributions is derived for arbitrarysystem sizes Nusing geometrical arguments in the system\u2019s con\ufb01guration space. For \ufb01nite systems, approxi-\nmate power-law behavior is obtained in the nonconservative regime, whereas for N!\u2018, critical behavior with\nan exponent of 23/2 is found in the conservative case only. We compare these results to the avalanche\nproperties found in networks of integrate-and-\ufb01re neurons, and relate the different dynamical regimes to theemergence of synchronization with and without oscillatory components.\nDOI: 10.1103/PhysRevE.66.066137 PACS number ~s!: 05.65. 1b, 05.70.Ln, 45.70.Ht, 87.18.Sn\nI. INTRODUCTION\nIn the last decade, a considerable number of publications\nhave been dedicated to the occurrence of power-law behaviorin systems involving interacting threshold elements drivenby slow external input. The dynamics accounts for phenom-ena occurring in such diverse systems as piles of granularmatter @1#, earthquakes @2#, the game of life @3#, friction @4#,\nand sound generated in the lung during breathing @5#.A n\navalanche of theoretical investigations was triggered by Bak,Tang, and Wiesenfeld @6#who linked the occurrence of\npower laws to the notion of self-organized criticality ~SOC!.\nIn the so-called sandpile models, locally connected elementsreceiving random input self-organize into a critical statecharacterized by power-law distributions of avalanches with-out the explicit tuning of a model parameter ~e.g., Refs.\n@7\u201318 #!. Analytical results were derived for sandpile models\n@14,15 #, and it was shown that the existence of a conserva-\ntion law is a necessary prerequisite to obtain SOC @16\u201318 #.\nA second class of models inspired by earthquake dynam-\nics employs continuous driving and nonconservative interac-tion between the elements of the system @4,19#. In the Olami-\nFeder-Christensen ~OFC!model @19#, where the amount of\ndissipation is controlled by a parameter\na, power-law behav-\nior of avalanches occurs for a wide range of avalues. Sub-\nsequent investigations emphasized the importance of bound-ary conditions and tied the existence of the observed scalingbehavior to synchronization phenomena induced by spatialinhomogeneities @20\u201324 #. More speci\ufb01cally, Lise and Jensen\n@25#introduced a random-neighbor interaction in the OFC\nmodel to avoid the buildup of spatial correlations. Furtheranalysis indeed revealed that the random-neighbor OFCmodel does not display SOC in the dissipative regime @26\u2013\n28#.\nIn these avalanche models with nonconservative interac-\ntion, analytical results have been obtained only for system\nsizeN!\u2018so far @26,29 #. Here we introduce a model that\nnot only circumvents the problem of system boundaries,", "doc_id": "b3e21c43-f122-4228-800c-1f3b373b3960", "embedding": null, "doc_hash": "d098bb5f2200807de284af0693d8ca5e48f9c980b95b8a1b438583a8dc241e95", "extra_info": null, "node_info": {"start": 0, "end": 3410}, "relationships": {"1": "950acfd7-35b6-40e0-bf25-1f85e4b3951d", "3": "ecd2b3d1-32cd-40e9-a2cb-2a1318531b90"}}, "__type__": "1"}, "ecd2b3d1-32cd-40e9-a2cb-2a1318531b90": {"__data__": {"text": "a wide range of avalues. Sub-\nsequent investigations emphasized the importance of bound-ary conditions and tied the existence of the observed scalingbehavior to synchronization phenomena induced by spatialinhomogeneities @20\u201324 #. More speci\ufb01cally, Lise and Jensen\n@25#introduced a random-neighbor interaction in the OFC\nmodel to avoid the buildup of spatial correlations. Furtheranalysis indeed revealed that the random-neighbor OFCmodel does not display SOC in the dissipative regime @26\u2013\n28#.\nIn these avalanche models with nonconservative interac-\ntion, analytical results have been obtained only for system\nsizeN!\u2018so far @26,29 #. Here we introduce a model that\nnot only circumvents the problem of system boundaries, butyields an analytical access also for \ufb01nite system sizes N. The\nelements are globally connected, which makes the system amean-\ufb01eld model. Randomness is not introduced throughrandom neighbors but by providing a random external input.During an avalanche, the elements become unstable and re-lax in a \ufb01xed order determined by the state of the systemimmediately prior to the avalanche. Therefore, the system is\nstrictly Abelian for dissipation parameters\nasmaller than a\nthreshold value, which can be readily worked out. In thiscase, a geometrical approach in the N-dimensional con\ufb01gu-\nration space yields an exact equation for the distribution ofavalanche sizes.\nIn Sec. II, the model is speci\ufb01ed and compared with other\ndissipative avalanche models, in particular, with the random-neighbor OFC model. In Sec. III, avalanche properties arepresented both numerically and analytically, whereby detailsof the analytical calculation of the avalanche size distribu-tions can be found in Appendixes A\u2013C. Extensions and ap-plications of the model are formulated in the terminology ofneural networks: The model allows for an interpretation interms of a fully connected neural network of nonleakyintegrate-and-\ufb01re neurons. Implications of this view such asthe synchronization behavior of local, densely connectedpopulations of cortical neurons will be discussed in Sec. IV.The paper concludes with a brief summary and discussion.\nII. THE AVALANCHE MODEL\nA. De\ufb01nition\nIn the model, time is measured in discrete steps, t\n50,1,2,....Consider a set of Nidentical threshold ele- *Electronic address: eurich@physik.uni-bremen.dePHYSICAL REVIEW E 66, 066137 ~2002!\n1063-651X/2002/66 ~6!/066137 ~15!/$20.00 \u00a92002 The American Physical Society 66066137-1\nments characterized by a state variable u>0, which will\nhenceforth be called energy. The system is initialized with\narbitrary values uiP@0,U)(i51 ,...,N), where Uis the\nthreshold above which elements become unstable and relax.\nDepending on the state of the system at time t, theith ele-\nment receives external input Iiext(t) or internal input Iiint(t)\nfrom other elements, resulting in an activation u\u02dcat timet\n11,\nu\u02dci~t11!5ui~t!1Iiext~t!1Iiint~t!. ~1!\nFrom the activation u\u02dci(t11), the energy of the ith ele-\nment at time t11 is computed as\nui~t11!5Hu\u02dci~t11!ifu\u02dci~t11!,U,\ne~u\u02dci~t11!2U!ifu\u02dci~t11!>U,~2!\ni.e., if the activation exceeds the threshold U, it is reset but\nretains a fraction e(0U,~2!\ni.e., if the activation exceeds the threshold U, it is reset but\nretains a fraction e(00 is de\ufb01ned\nto be the smallest integer for which the stopping condition\nM(t\n01D)50 is satis\ufb01ed. The avalanche size Lis given by\nL5(k50D21M(t01k). The model allows the calculation of the\nprobability P(L,N,a) of an avalanche of size L>0 in the\nregime 0 1,\nwhich is related to P(L,N,a) via\np~L,N,a![P~L,N,a!\n12P~0,N,a!. ~3!\nAvalanche duration distributions will be denoted by\npd(D,N,a)(D>1).Due to the global coupling of the elements, there are no\nboundary conditions to be speci\ufb01ed in the model.\nB. The case e\u02dc1\nBoth the coupling parameter aand the reset parameter e\ncontrol the amount of dissipation in the system.An analytical\napproach will be possible for e51, that is, if all suprathresh-\nold elements are reset such that they lose an identical amountUof energy @cf. Eq. ~2!#. We will therefore restrict further\nanalysis to this case and only brie\ufb02y return to the generalsituation in Sec. IV.\nFor\ne51, the value a51 corresponds to the conservative\ncase with respect to the internal dynamics: upon resetting ofa suprathreshold element, the energy it loses is completely\ndistributed in the network. For\na>1, an in\ufb01nite avalanche\nmay eventually occur and we will therefore restrict ourselves\nto the case", "doc_id": "b2006ef0-2c96-48f2-b5a4-9f5ecebab917", "embedding": null, "doc_hash": "a440d7b733705c8d893d807288782fab81aef68d9447049c7d078521883697bb", "extra_info": null, "node_info": {"start": 6328, "end": 9320}, "relationships": {"1": "950acfd7-35b6-40e0-bf25-1f85e4b3951d", "2": "ecd2b3d1-32cd-40e9-a2cb-2a1318531b90", "3": "4d4caa9d-39d9-4341-8719-5c55510fc86f"}}, "__type__": "1"}, "4d4caa9d-39d9-4341-8719-5c55510fc86f": {"__data__": {"text": "the coupling parameter aand the reset parameter e\ncontrol the amount of dissipation in the system.An analytical\napproach will be possible for e51, that is, if all suprathresh-\nold elements are reset such that they lose an identical amountUof energy @cf. Eq. ~2!#. We will therefore restrict further\nanalysis to this case and only brie\ufb02y return to the generalsituation in Sec. IV.\nFor\ne51, the value a51 corresponds to the conservative\ncase with respect to the internal dynamics: upon resetting ofa suprathreshold element, the energy it loses is completely\ndistributed in the network. For\na>1, an in\ufb01nite avalanche\nmay eventually occur and we will therefore restrict ourselves\nto the case a,1. In order to avoid side effects resulting\nfrom the null set of rational values of a,U,o rDU,w e\nassume one of the fractions a/UorDU/Uto be irrational.\nAs will be shown below, a variation of aleads to qualita-\ntively different avalanche size distributions.\nC. Comparison with other avalanche models\nAclass of models discussed in the SOC literature employs\na parameter controlling the amount of dissipation @4,19\u201328 #.\nThe numerically observed power-law behavior in such sys-tems, however, could be ascribed to spatial inhomogeneitiesand the employed boundary conditions ~e.g., @21\u201324 #!.I n\norder to study avalanches of activity in the presence of dis-sipation independent of spatial correlations among elements,Lise and Jensen @25#introduced a random-neighbor version\nof the Olami-Feder-Christensen model described in Ref.@19#. In this model, threshold elements receive a constant,\nuniform input and have random nearest neighbors to whichthey are connected during an avalanche. The temporal vari-ability of the network connectivity avoids the buildup of spa-tial correlations, thus ruling out boundary effects in shapingavalanche distributions. Subsequent studies, however, dem-onstrated that the random-neighbor OFC model does nothave scaling behavior in the dissipative regime @26\u201328 #.\nBro\u00a8ker and Grassberger @26#, in their analytical consider-\nations of the random-neighbor OFC model, applied thetheory of branching processes to yield avalanche size distri-butions. For this purpose it was necessary to consider the\nlimitsd!\u2018~wheredis the dimension of the lattice !and\nN!\u2018in order to make the model effectively Abelian and\navoid correlations among elements @26#. This prevents ava-\nlanches from visiting elements more than once and allowssubavalanches to spread independently of each other suchthat each suprathreshold element has a distinctive predeces-sor which triggered it.\nOur model poses an alternative of the random-neighbor\nOFC model: the global coupling of elements prevents spatialcorrelations and the putative dependence of the system be-havior on boundary conditions. Randomness is introducedthrough the external input rather than the random assignmentof nearest neighbors. This approach has the advantage of not\nrequiring the limit N!\u2018: For\ne51, the system is AbelianEURICH, HERRMANN, AND ERNST PHYSICAL REVIEW E 66, 066137 ~2002!\n066137-2\nfor an arbitrary system size Nbecause at each time step t\nduring an avalanche, all elements receive the same input de-\npending only on the number M(t21) of suprathreshold ele-\nments at time t21.\nThe random-neighbor OFC model and the globally\ncoupled model are complementary in the following sense: inthe random-neighbor OFC model, randomness is introducedthrough the random choice of neighbors during the ava-lanche activity, while the interavalanche dynamics is a\nsimple shift of the energy distribution\nr(u) on theuaxis due\nto the uniform input. In our globally coupled", "doc_id": "4d4caa9d-39d9-4341-8719-5c55510fc86f", "embedding": null, "doc_hash": "4997f4928a0d7b04b9bdca09e7d2d2d84735a83b981d4e994af437f4c780374d", "extra_info": null, "node_info": {"start": 9139, "end": 12760}, "relationships": {"1": "950acfd7-35b6-40e0-bf25-1f85e4b3951d", "2": "b2006ef0-2c96-48f2-b5a4-9f5ecebab917", "3": "4753dd74-9764-40be-8baa-81348163e0bd"}}, "__type__": "1"}, "4753dd74-9764-40be-8baa-81348163e0bd": {"__data__": {"text": "the system is AbelianEURICH, HERRMANN, AND ERNST PHYSICAL REVIEW E 66, 066137 ~2002!\n066137-2\nfor an arbitrary system size Nbecause at each time step t\nduring an avalanche, all elements receive the same input de-\npending only on the number M(t21) of suprathreshold ele-\nments at time t21.\nThe random-neighbor OFC model and the globally\ncoupled model are complementary in the following sense: inthe random-neighbor OFC model, randomness is introducedthrough the random choice of neighbors during the ava-lanche activity, while the interavalanche dynamics is a\nsimple shift of the energy distribution\nr(u) on theuaxis due\nto the uniform input. In our globally coupled model, thestochasticity is due to the random external input betweenavalanches, whereas the avalanche activity corresponds to a\nrotation of\nr(u) on a circle @0,U) with periodic boundary\nconditions. The latter property is due to ~i!the fact that all\nelements\u2014including the unstable ones\u2014receive the same in-\nputIiint(t) at each time step, and ~ii!the update rule ~2!which\nreinjects unstable elements according to the suprathreshold\nportionu\u02dci(t11)2Uof their energy. Therefore, the elements\nbecome unstable in a \ufb01xed order depending on the actual\ndistribution r(u). Below it will be shown that for coupling\ncoef\ufb01cients a,max$12DU/U,N/(N11)%, avalanche sizes\nmay not exceed N, which means that each element can be\nactivated only once. In this regime, avalanche distributionsturn out to be very similar for the random-neighbor OFCmodel and the current model, demonstrating that the differ-ences between the models barely change the statistical prop-\nerties of the avalanches. However, in the globally coupledmodel, this regime can be described by a closed expression\nfor avalanche distributions, p(L,N,\na).\nIII. AVALANCHE PROPERTIES\nA. Avalanche sizes\nFigure 1 shows avalanche size distributions for different\nvalues of a.N510000 was chosen as the system size, but\nthe curves look very similar for any other choice of N.\nFour qualitatively different regimes can be distinguished\nwhich will be termed subcritical, critical, supracritical, and\nmultipeaked. For small values of a, subcritical avalanche\nsize distributions exist, which can be approximated by thegeneral expression\np\n~L,N,a!\u2019p\u02c6~L,N,a!5Lgexp~2L/l!, ~4!\nwhere gis an exponent independent of Nto be characterized\nbelow, and l5l(N,a) describes the range of avalanche\nsizes over which power-law behavior is observed @Fig. 1 ~a!#.\nFor \ufb01xed N,l(N,a) is a monotonically increasing function\nofaas long as a,acwhich we refer to as the \u2018\u2018critical\ncase\u2019\u2019 ~Fig. 2 !. For ac, the system has avalanche distribu-\ntions with an approximate power-law behavior with expo-\nnent 23/2 from L51 almost up to the size of the system,\nwhere the usual exponential cutoff is observed @49#@Fig.\n1~b!#. For \ufb01nite N,acis in the dissipative regime.Above the\ncritical value ac, avalanche size distributions become non-\nmonotonic @Fig. 1 ~c!#. Such supracritical curves have a mini-\nmum at some intermediate avalanche size.\nIn order to \ufb01nd the critical coupling coef\ufb01cient acas a\nfunction of system size N, we computed a conveniently de-\n\ufb01ned distance K(a) between the distribution p(L,N,a) and\nFIG. 1. Probability distributions of avalanche sizes, p(x,N,a),\nand avalanche durations,", "doc_id": "4753dd74-9764-40be-8baa-81348163e0bd", "embedding": null, "doc_hash": "dc1d91cfe2474537aca56dea190192ed6d6119b9b20370fc8a9c529d2e6c9aeb", "extra_info": null, "node_info": {"start": 12777, "end": 16049}, "relationships": {"1": "950acfd7-35b6-40e0-bf25-1f85e4b3951d", "2": "4d4caa9d-39d9-4341-8719-5c55510fc86f", "3": "27891564-af8b-4c1b-b331-bae9cd5f0d38"}}, "__type__": "1"}, "27891564-af8b-4c1b-b331-bae9cd5f0d38": {"__data__": {"text": "from L51 almost up to the size of the system,\nwhere the usual exponential cutoff is observed @49#@Fig.\n1~b!#. For \ufb01nite N,acis in the dissipative regime.Above the\ncritical value ac, avalanche size distributions become non-\nmonotonic @Fig. 1 ~c!#. Such supracritical curves have a mini-\nmum at some intermediate avalanche size.\nIn order to \ufb01nd the critical coupling coef\ufb01cient acas a\nfunction of system size N, we computed a conveniently de-\n\ufb01ned distance K(a) between the distribution p(L,N,a) and\nFIG. 1. Probability distributions of avalanche sizes, p(x,N,a),\nand avalanche durations, pd(x,N,a), in the subcritical @~a!,a\n50.8], critical @~b!,a50.99], supracritical @~c!,a50.999], and\nmultipeaked @~d!,a50.99997] regime. ~a!\u2013~c!Solid lines and\nsymbols denote the analytical and the numerical results for the ava-lanche size distributions, respectively. In ~d!, the solid line shows\nthe numerically calculated avalanche size distribution. The dashedlines in ~a!\u2013~d!show the numerically evaluated avalanche duration\ndistributions. In all cases, the presented curves are temporal aver-ages over 10\n7avalanches with N510000, DU50.022, and U\n51.\nFIG.2. Range l(N,a) ofavalanchesizesoverwhichpower-law\nbehavior is observed in the subcritical regime. l(N,a) has been\nplotted for four different system sizes, namely, for N5102~solid\nline!,N5103~dashed line !,N5104~dashed-dotted line !, andN\n5105~dotted line !.To obtain l,p\u02c6(L,N,a) as de\ufb01ned in Eq. ~4!has\nbeen \ufb01tted to the analytically calculated avalanche size distribution\np(L,N,a) by maximizing the symmetric version of the Kullback-\nLeibler distance K(l) as de\ufb01ned by K(l)5(L(p2p\u02c6)@ln(p)\n2ln(p\u02c6)#.FINITE-SIZE EFFECTS OF AVALANCHE DYNAMICS PHYSICAL REVIEW E 66, 066137 ~2002!\n066137-3\nan \u2018\u2018ideal\u2019\u2019 power-law distribution p\u02dc(L,N)5L23/2/(LL23/2.\nThenK(a) was numerically minimized to yield the param-\neteracfor which the distribution is closest to a power law.\nWe chose the symmetric version of the Kullback-Leibler dis-\ntance as de\ufb01ned by K(a)5(L(p2p\u02dc)@ln(p)2ln(p\u02dc)#, which\nrevealed a critical coupling constant\nac~N!\u201912N2mwith m50.560.01 ~5!\n~obtained for system sizes ranging from N5102up toN\n5107). An alternative approach to obtain the exponent mis\nto compute the slope of the avalanche size distribution\np(L,N,a) for avalanche sizes L5N/2 using the analytical\nexpression to be derived below. The result is m50.5, in\nagreement with the numerics.\nAbove the supracritical case, a fourth regime exists for\nvalues of aclose to 1, where the distributions show multiple\npeaks located at L5N,2N11,3N11 ,....These peaks arise\nfrom the high coupling strength because elements can be-come suprathreshold more than only once during an ava-lanche. This is not possible in the subcritical, critical, andsupracritical regimes. Figure 1 ~d!shows an example with\nthree peaks ~note that the last maximum is not referred to as\na peak !.\nConditions for the occurrence of", "doc_id": "27891564-af8b-4c1b-b331-bae9cd5f0d38", "embedding": null, "doc_hash": "3defb0441bbacc24d7af3eec133fae96aad0894cf8f2d61aa5d4b36ea8f539e9", "extra_info": null, "node_info": {"start": 16116, "end": 19019}, "relationships": {"1": "950acfd7-35b6-40e0-bf25-1f85e4b3951d", "2": "4753dd74-9764-40be-8baa-81348163e0bd", "3": "67231d57-e066-4cda-84fe-b3df6c8e09a8"}}, "__type__": "1"}, "67231d57-e066-4cda-84fe-b3df6c8e09a8": {"__data__": {"text": "compute the slope of the avalanche size distribution\np(L,N,a) for avalanche sizes L5N/2 using the analytical\nexpression to be derived below. The result is m50.5, in\nagreement with the numerics.\nAbove the supracritical case, a fourth regime exists for\nvalues of aclose to 1, where the distributions show multiple\npeaks located at L5N,2N11,3N11 ,....These peaks arise\nfrom the high coupling strength because elements can be-come suprathreshold more than only once during an ava-lanche. This is not possible in the subcritical, critical, andsupracritical regimes. Figure 1 ~d!shows an example with\nthree peaks ~note that the last maximum is not referred to as\na peak !.\nConditions for the occurrence of kpeaks in the avalanche\nsize distributions can be readily worked out. Consider the\ncasek51 corresponding to the situation that neurons may\n\ufb01re twice at most during an avalanche. First, an avalanche\nsizeL5N11 must be possible. Since all elements receive\nthe same internal input and \ufb01re in a \ufb01xed order as describedabove, this is equivalent to the condition that the elementwhich originally triggered the avalanche may \ufb01re twice. Af-terN\ufb01ring events, this element has received the total input\nDU1\naU. A second \ufb01ring can thus occur if this input ex-\nceeds the threshold, or a.12DU/U. Second, after N11\n\ufb01ring events, the total internal input to each element must\nexceed the threshold to allow for further \ufb01ring, ( N\n11)aU/N.Uora.N/(N11). Similar arguments hold\nfor the general case of kpeaks. The above conditions must\nthen be replaced by\na.amin~k!5maxH12DU\nkU,kN\nkN11J. ~6!\namin(k),aluk/m,Ais nonempty if and only if\nIk,m\\Jl,m5B; and this implies that Ik,m#Jl,m,A\u00deB. Note\nthat ifk.l, condition Ik,m#Jl,mis never ful\ufb01lled.\nLemma 2.", "doc_id": "701d0aff-6665-4b22-98b5-4bd41470f1db", "embedding": null, "doc_hash": "5664f702c503e98901ae466b2f5b76b027003ec81c92883f03bce55f71e01d3c", "extra_info": null, "node_info": {"start": 48125, "end": 50039}, "relationships": {"1": "950acfd7-35b6-40e0-bf25-1f85e4b3951d", "2": "30fa272d-b0ff-4b7f-b7cb-17f3e098b8bd", "3": "f5f3457d-3d38-45f9-bea0-60efa8549999"}}, "__type__": "1"}, "f5f3457d-3d38-45f9-bea0-60efa8549999": {"__data__": {"text": "~A1!,~A3!, and ~A5!, we can then explicitly\nwriteAas\nA5$xPRmu0luk/m,Ais nonempty if and only if\nIk,m\\Jl,m5B; and this implies that Ik,m#Jl,m,A\u00deB. Note\nthat ifk.l, condition Ik,m#Jl,mis never ful\ufb01lled.\nLemma 2. ;l