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Gossiping has been considered intensively for butterflies and “simple” butterflies (which have no wrap-around connections). In the “telephone” communication model, for a butterfly of order k, the best previous gossiping algorithms require 212k and 3k communication rounds, respectively. By new asymptotic methods we break through these bounds. We show that gossiping on a class of “column-based” networks, which also contains the cube-connected cycles, can be reduced to the simpler problem of “row-gossiping”. Row-gossiping in turn is reduced to “coherent row-broadcasting”. This latter problem is sufficiently simple to be solved by a sophisticated computer program for butterflies with up to 15×215 nodes. Out of the produced solutions a pattern is distilled, which can be used to perform gossiping on butterflies and simple butterflies of order k in 214k+o(k) and 212k+o(k) rounds, respectively, for any k, considerably reducing the gap with the lower bounds. The new upper bounds also hold for gossiping in the weaker “telegraph” model.  相似文献   

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In this paper we discuss the blow-up for classical solutions to the following class of parabolic equations with Robin boundary condition: {(b(u))t=??(g(u)?u)+f(u)in  Ω×(0,T),?u?n+γu=0on  ?Ω×(0,T),u(x,0)=h(x)0in  Ω¯, where Ω is a bounded domain of RN(N2) with smooth boundary ?Ω. By constructing some appropriate auxiliary functions and using a first-order differential inequality technique, we derive conditions on the data which guarantee the blow-up or the global existence of the solution. For the blow-up solution, a lower bound on blow-up time is also obtained. Moreover, some examples are presented to illustrate the applications.  相似文献   

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We prove for three-dimensional domains the existence of local strong solutions to systems of nonlinear partial differential equations with p()-structure, pp()p0, and Dirichlet boundary conditions for p>95 without restriction on the upper bound p0. In particular this result is applicable to the motion of electrorheological fluids.  相似文献   

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In this paper, we consider the blow-up criterion for the quasi-geostrophic equations with dissipation Λγ (0<γ<1). By establishing a new trilinear estimate, we show that if
θLγγ+s?1(0,T;B?,s(R2))
for some s1?γ2,1, then the solution can be extended smoothly past T. This improves and extends the corresponding results in Dong and Pavlovi? (2009) ([32]) and Yuan (2010).  相似文献   

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