Abstract

Abstract This paper deals with the large time behavior of non-negative solutions for the porous medium equation with a nonlinear gradient source u t = Δ u m + | ∇ u l | q , ( x , t ) ∈ Ω × ( 0 , ∞ ) , where l ≥ m > 1 and 1 ≤ q < 2 . When l q = m , we prove that the global solution converges to the separate variable solution t − 1 m − 1 f ( x ) . While m < l q ≤ m + 1 , we note that the global solution converges to the separate variable solution t − 1 m − 1 f 0 ( x ) . Moreover, when l q > m + 1 , we show that the global solution also converges to the separate variable solution t − 1 m − 1 f 0 ( x ) for the small initial data u 0 ( x ) , and we find that the solution u ( x , t ) blows up in finite time for the large initial data u 0 ( x ) . MSC:35K55, 35K65, 35B40.

Highlights

  • 1, we show that the global solution converges to the separate variable solution t

  • 1 Introduction In this paper, we investigate the large time behavior of non-negative solutions for the following initial-boundary value problem:

  • In [ ], Andreucci proved the existence of solutions for the following degenerate parabolic equation with initial data measures: ut = um + |∇ul|q, (x, t) ∈ RN × (, ∞), u(x, ) = μ, x ∈ RN, ( . )

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Summary

Introduction

1 Introduction In this paper, we investigate the large time behavior of non-negative solutions for the following initial-boundary value problem: In [ ], Andreucci proved the existence of solutions for the following degenerate parabolic equation with initial data measures: ut = um + |∇ul|q, (x, t) ∈ RN × ( , ∞), u(x, ) = μ, x ∈ RN , For the special case m = l = , Gilding [ ] studied the large time behavior of solutions to the following Cauchy problem: ut = u + |∇u|q, (x, t) ∈ RN × ( , ∞), u(x, ) = u (x), x ∈ RN , Barles et al [ ] studied the large time behavior of solutions for the following initial-boundary value problem:

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