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1.
We study the Cauchy problem for the nonlinear dissipative equations (0.1) uo∂u-αδu + Β|u|2/n u = 0,x ∃ Rn,t } 0,u(0,x) = u0(x),x ∃ Rn, where α,Β ∃ C, ℜα 0. We are interested in the dissipative case ℜα 0, and ℜδ(α,Β) 0, θ = |∫ u0(x)dx| ⊋ 0, where δ(α, Β) = ##|α|n-1nn/2 / ((n + 1)|α|2 + α2 n/2. Furthermore, we assume that the initial data u0 ∃ Lp are such that (1 + |x|)αu0 ∃ L1, with sufficiently small norm ∃ = (1 + |x|)α u0 1 + u0 p, wherep 1, α ∃ (0,1). Then there exists a unique solution of the Cauchy problem (0.1)u(t, x) ∃ C ((0, ∞); L) ∩ C ([0, ∞); L1 ∩ Lp) satisfying the time decay estimates for allt0 u(t)|| Cɛt-n/2(1 + η log 〈t〉)-n/2, if hg = θ2/n 2π ℜδ(α, Β) 0; u(t)|| Cɛt-n/2(1 + Μ log 〈t〉)-n/4, if η = 0 and Μ = θ4/n 4π)2 (ℑδ(α, Β))2 ℜ((1 + 1/n) υ1-1 υ2) 0; and u(t)|| Cɛt-n/2(1 + κ log 〈t〉)-n/6, if η = 0, Μ = 0, κ 0, where υl,l = 1,2 are defined in (1.2), κ is a positive constant defined in (2.31).  相似文献   

2.
We study Lp decay estimates of the solution to the Cauchy problem for the dissipative wave equation in even dimensions: (□+?t)u=0 in ?N × (0,∞) for even N=2n?2 with initial data (u,?tu)∣t=0 =(u0,u1). The representation formulas of the solution u(t)=?tS(t)u0 + S(t)(u0+u1) provide the sharp estimates on Lp norms with p?1. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   

3.
The properties of solutions of the equationu″(t) =p 1(t)u1(t)) +p 2(t)u′(τ2(t)) are investigated wherep i :a, + ∞[→R (i=1,2) are locally summable functions τ1 :a, + ∞[→R is a measurable function, and τ2 :a, + ∞[→R is a nondecreasing locally absolutely continuous function. Moreover, τ i (t) ≥t (i = 1,2),p 1(t)≥0,p 2 2 (t) ≤ (4 - ɛ)τ 2 (t)p 1(t), ɛ =const > 0 and . In particular, it is proved that solutions whose derivatives are square integrable on [α,+∞] form a one-dimensional linear space and for any such solution to vanish at infinity it is necessary and sufficient that .  相似文献   

4.
Consider the Cauchy problem in odd dimensions for the dissipative wave equation: (□+∂t)u=0 in with (u,∂tu)|t=0=(u0,u1). Because the L2 estimates and the L estimates of the solution u(t) are well known, in this paper we pay attention to the Lp estimates with 1p<2 (in particular, p=1) of the solution u(t) for t0. In order to derive Lp estimates we first give the representation formulas of the solution u(t)=∂tS(t)u0+S(t)(u0+u1) and then we directly estimate the exact solution S(t)g and its derivative ∂tS(t)g of the dissipative wave equation with the initial data (u0,u1)=(0,g). In particular, when p=1 and n1, we get the L1 estimate: u(t)L1Cet/4(u0Wn,1+u1Wn−1,1)+C(u0L1+u1L1) for t0.  相似文献   

5.
We investigate the existence of nonnegative weak solutions to the problem ut=Δ(um)−p|∇u| in Rn×(0,∞) with +(1−2/n)<m<1. It will be proved that: (i) When 1<p<2, if the initial datum u0D(Rn) then there exists a solution; (ii) When 1<p<(2+mn)/(n+1), if the initial datum u0(x) is a bounded and nonnegative measure then the solution exists; (iii) When (2+mn)/(n+1)?p<2, if the initial datum is a Dirac mass then the solution does not exist. We also study the large time behavior of the L1-norm of solutions for 1<p?(2+mn)/(n+1), and the large time behavior of t1/βu(⋅,t)−Ec(⋅,t)L for (2+mn)/(n+1)<p<2.  相似文献   

6.
We consider nonnegative solutions of initial-boundary value problems for parabolic equationsu t=uxx, ut=(um)xxand (m>1) forx>0,t>0 with nonlinear boundary conditions−u x=up,−(u m)x=upand forx=0,t>0, wherep>0. The initial function is assumed to be bounded, smooth and to have, in the latter two cases, compact support. We prove that for each problem there exist positive critical valuesp 0,pc(withp 0<pc)such that forp∃(0,p 0],all solutions are global while forp∃(p0,pc] any solutionu≢0 blows up in a finite time and forp>p csmall data solutions exist globally in time while large data solutions are nonglobal. We havep c=2,p c=m+1 andp c=2m for each problem, whilep 0=1,p 0=1/2(m+1) andp 0=2m/(m+1) respectively. This work was done during visits of the first author to Iowa State University and the Institute for Mathematics and its Applications at the University of Minnesota. The second author was supported in part by NSF Grant DMS-9102210.  相似文献   

7.
In this paper we consider the Cauchy problem for the equation ∂u/∂t + uu/∂x + u/x = 0 for x > 0, t ⩾ 0, with u(x, 0) = u0(x) for x < x0, u(x, 0) = u0+(x) for x > x0, u0(x0) > u0+(x0). Following the ideas of Majda, 1984 and Lax, 1973, we construct, for smooth u0 and u0+, a global shock front weak solution u(x, t) = u(x, t) for x < ϕ(t), u(x, t) = u+(x, t) for x > ϕ(t), where u and u+ are the strong solutions corresponding (respectively) to u0 and u0+ and the curve t → ϕ(t) is defined by dϕ/dt (t) = 1/2[u(ϕ(t), t) + u+(ϕ(t), t)], t ⩾ 0 and ϕ(0) = x0. © 1998 B. G. Teubner Stuttgart—John Wiley & Sons, Ltd.  相似文献   

8.
It is established that the linear problemu u a 2 u xx =g(x,t),u(0,t) =u(x, t + T) =u(x,t) is always solvable in the function spaceA = {g:g(x,t) =g(x,t+T) =g( –x,t) = –g(–x,t)} provided thataTq = (2p – 1) and (2p – 1,q) = 1, wherepandq are integer numbers. To prove this statement, an exact solution is constructed in the form of an integral operator, which is used to prove the existence of a solution of a periodic boundary-value problem for a nonlinear second-order wave equation. The results obtained can be used when studying the solutions to nonlinear boundary-value problems by asymptotic methods.Translated from Ukrainskii Matematicheskii Zhurnal, Vol. 45, No. 8, pp. 1115–1121, August, 1993.  相似文献   

9.
10.
In this paper, we consider the unboundedness of solutions of the following differential equation (φp(x′))′ + (p ? 1)[αφp(x+) ? βφp(x?)] = f(x)x′ + g(x) + h(x) + e(t) where φp(u) = |u|p? 2 u, p > 1, x± = max {±x, 0}, α and β are positive constants satisfying with m, nN and (m, n) = 1, f and g are continuous and bounded functions such that limx→±∞g(x) ? g(±∞) exists and h has a sublinear primitive, e(t) is 2πp‐periodic and continuous. (© 2004 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)  相似文献   

11.
In this paper, we study the initial-boundary value problem of porous medium equation ρ(x)u t  = Δu m  + V(x)h(t)u p in a cone D = (0, ∞) × Ω, where V(x)  ~  |x|s, h(t)  ~  ts{V(x)\,{\sim}\, |x|^\sigma, h(t)\,{\sim}\, t^s}. Let ω 1 denote the smallest Dirichlet eigenvalue for the Laplace-Beltrami operator on Ω and let l denote the positive root of l 2 + (n − 2)l = ω 1. We prove that if m < p £ 1+(m-1)(1+s)+\frac2(s+1)+sn+l{m < p \leq 1+(m-1)(1+s)+\frac{2(s+1)+\sigma}{n+l}}, then the problem has no global nonnegative solutions for any nonnegative u 0 unless u 0 = 0; if ${p >1 +(m-1)(1+s)+\frac{2(s+1)+\sigma}{n+l}}${p >1 +(m-1)(1+s)+\frac{2(s+1)+\sigma}{n+l}}, then the problem has global solutions for some u 0 ≥ 0.  相似文献   

12.
We consider the periodic boundary-value problem u tt u xx = g(x, t), u(0, t) = u(π, t) = 0, u(x, t + ω) = u(x, t). By representing a solution of this problem in the form u(x, t) = u 0(x, t) + ũ(x, t), where u 0(x, t) is a solution of the corresponding homogeneous problem and ũ(x, t) is the exact solution of the inhomogeneous equation such that ũ(x, t + ω) u x = ũ(x, t), we obtain conditions for the solvability of the inhomogeneous periodic boundary-value problem for certain values of the period ω. We show that the relation obtained for a solution includes known results established earlier. __________ Translated from Ukrains'kyi Matematychnyi Zhurnal, Vol. 57, No. 7, pp. 912–921, July, 2005.  相似文献   

13.
Parabolic partial differential equations with overspecified data play a crucial role in applied mathematics and engineering, as they appear in various engineering models. In this work, the radial basis functions method is used for finding an unknown parameter p(t) in the inverse linear parabolic partial differential equation ut = uxx + p(t)u + φ, in [0,1] × (0,T], where u is unknown while the initial condition and boundary conditions are given. Also an additional condition ∫01k(x)u(x,t)dx = E(t), 0 ≤ tT, for known functions E(t), k(x), is given as the integral overspecification over the spatial domain. The main approach is using the radial basis functions method. In this technique the exact solution is found without any mesh generation on the domain of the problem. We also discuss on the case that the overspecified condition is in the form ∫0s(t) u(x,t)dx = E(t), 0 < tT, 0 < s(t) < 1, where s and E are known functions. Some illustrative examples are presented to show efficiency of the proposed method. © 2007 Wiley Periodicals, Inc. Numer Methods Partial Differential Eq, 2007  相似文献   

14.
This paper deals with the Cauchy problem utuxx + up = 0; − ∞ < x < + ∞, t>0, u(x, 0) = u0(x); − ∞ < x < + ∞, where 0 < p < 1 and u0(x) is continuous, nonnegative, and bounded. In this case, solutions are known to vanish in a finite time T, and interfaces separating the regions where u(x, t) > 0 and u(x, t) = 0 appear when t is close to T. We describe here all possible asymptotic behaviours of solutions and interfaces near an extinction point as the extinction time is approached. We also give conditions under which some of these behaviours actually occur.  相似文献   

15.
This paper considers the existence and large time behavior of solutions to the convection-diffusion equation u t −Δu+b(x)·∇(u|u| q −1)=f(x, t) in ℝ n ×[0,∞), where f(x, t) is slowly decaying and q≥1+1/n (or in some particular cases q≥1). The initial condition u 0 is supposed to be in an appropriate L p space. Uniform and nonuniform decay of the solutions will be established depending on the data and the forcing term.This work is partially supported by an AMO Grant  相似文献   

16.
In this paper, the boundedness of all solutions of the nonlinear differential equation (φp(x′))′ + αφp(x+) – βφp(x) + f(x) = e(t) is studied, where φp(u) = |u|p–2 u, p ≥ 2, α, β are positive constants such that = 2w–1 with w ∈ ?+\?, f is a bounded C5 function, e(t) ∈ C6 is 2πp‐periodic, x+ = max{x, 0}, x = max{–x, 0}. (© 2004 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)  相似文献   

17.
In the paper, we obtain the existence of symmetric or monotone positive solutions and establish a corresponding iterative scheme for the equation (ϕ p (u′))′+q(t)f(u) = 0, 0 < t < 1, where ϕ p (s):= |s| p−2 s, p > 1, subject to nonlinear boundary condition. The main tool is the monotone iterative technique. Here, the coefficient q(t) may be singular at t = 0; 1.  相似文献   

18.
For the equation K(t)u xx + u tt b 2 K(t)u = 0 in the rectangular domain D = “(x, t)‖ 0 < x < 1, −α < t < β”, where K(t) = (sgnt)|t| m , m > 0, and b > 0, α > 0, and β > 0 are given real numbers, we use the spectral method to obtain necessary and sufficient conditions for the unique solvability of the boundary value problem u(0, t) = u(1, t), u x (0, t) = u x (1, t), −αtβ, u(x, β) = φ(x), u(x,−α) = ψ(x), 0 ≤ x ≤ 1.  相似文献   

19.
We investigate the large-time behaviour of solutions to the nonlinear heat-conduction equation with absorption ut = Δ(uσ + 1) − uβ in Q = RN × (0, ∞) (E) with N 1, σ > 0 and critical absorption exponent β = σ + 1 + 2/N; the initial function u(x, 0) = 0 is assumed to be integrable, nonnegative and compactly supported. We prove that u converges as t → ∞ to a unique self-similar function which is a contracted version of one of the asymptotic profiles of the nonabsorptive problem ut = Δ(uσ + 1), the same for any initial data. The cornerstone of the proof is a result about ω-limits of (infinite-dimensional) asymptotical dynamical systems. Combining this result with an asymptotic evaluation of the mass function as well as typical PDE estimates gives the behaviour of (E) for large times.Similar unusual asymptotic behaviour is obtained for the equation ut = div(¦Du¦σ Du) − uβ with same conditions on σ and u(x, 0) and critical value for β = σ + 1 + (σ + 2)/N.  相似文献   

20.
Existence theorems for the nonlinear parabolic differential equation −∂u/∂t + Δu + |u|p + f(x, t) = 0 in n × [0, ∞) with zero initial value are established given explicit conditions on the nonhomogeneous termf(x, t). An existence theorem is also demonstrated for the corresponding elliptic equation.  相似文献   

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