<p>This paper is concerned with the local and global properties of nonnegative solutions for semilinear heat equation <InlineEquation ID="IEq1"> <InlineMediaObject> <ImageObject Color="BlackWhite" FileRef="526_2024_2907_Article_IEq1.gif" Format="GIF" Height="19" Rendition="HTML" Resolution="72" Type="Linedraw" Width="176" /> </InlineMediaObject> <EquationSource Format="TEX">\(u_t-\Delta u=u^p+M|\nabla u|^q\)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <msub> <mi>u</mi> <mi>t</mi> </msub> <mo>-</mo> <mi mathvariant="normal">Δ</mi> <mi>u</mi> <mo>=</mo> <msup> <mi>u</mi> <mi>p</mi> </msup> <mo>+</mo> <mi>M</mi> <msup> <mrow> <mo stretchy="false">|</mo> <mi mathvariant="normal">∇</mi> <mi>u</mi> <mo stretchy="false">|</mo> </mrow> <mi>q</mi> </msup> </mrow> </math></EquationSource> </InlineEquation> in <InlineEquation ID="IEq2"> <InlineMediaObject> <ImageObject Color="BlackWhite" FileRef="526_2024_2907_Article_IEq2.gif" Format="GIF" Height="18" Rendition="HTML" Resolution="72" Type="Linedraw" Width="119" /> </InlineMediaObject> <EquationSource Format="TEX">\(\Omega \times I\subset \mathbb {R}^N\times \mathbb {R}\)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi mathvariant="normal">Ω</mi> <mo>×</mo> <mi>I</mi> <mo>⊂</mo> <msup> <mrow> <mi mathvariant="double-struck">R</mi> </mrow> <mi>N</mi> </msup> <mo>×</mo> <mi mathvariant="double-struck">R</mi> </mrow> </math></EquationSource> </InlineEquation>, where <InlineEquation ID="IEq3"> <InlineMediaObject> <ImageObject Color="BlackWhite" FileRef="526_2024_2907_Article_IEq3.gif" Format="GIF" Height="14" Rendition="HTML" Resolution="72" Type="Linedraw" Width="50" /> </InlineMediaObject> <EquationSource Format="TEX">\(M&gt;0\)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi>M</mi> <mo>&gt;</mo> <mn>0</mn> </mrow> </math></EquationSource> </InlineEquation>, and <InlineEquation ID="IEq4"> <InlineMediaObject> <ImageObject Color="BlackWhite" FileRef="526_2024_2907_Article_IEq4.gif" Format="GIF" Height="16" Rendition="HTML" Resolution="72" Type="Linedraw" Width="57" /> </InlineMediaObject> <EquationSource Format="TEX">\(p,q&gt;1\)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi>p</mi> <mo>,</mo> <mi>q</mi> <mo>&gt;</mo> <mn>1</mn> </mrow> </math></EquationSource> </InlineEquation>. We first establish the local pointwise gradient estimates when <i>q</i> is subcritical, critical and supercritical with respect to <i>p</i>. With these estimates, we can prove the parabolic Liouville-type theorems for time-decreasing ancient solutions. Next, we use Gidas–Spruck type integral methods to prove the Liouville-type theorem for the entire solutions when <i>q</i> is critical. Finally, as an application of the Liouville-type theorem, we use the doubling lemma to derive universal priori estimates for local solutions of parabolic equations with general nonlinearities. Our approach relies on a parabolic differential inequality containing a suitable auxiliary function rather than Keller–Osserman type inequality, which allows us to generalize and extend the partial results of the elliptic equation (Bidaut-Véron et al. in Math. Ann. 378(1–2):13–56, 2020) to the parabolic case.</p>

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A priori estimates and Liouville-type theorems for the semilinear parabolic equations involving the nonlinear gradient source

  • Wenguo Liang,
  • Zhengce Zhang

摘要

This paper is concerned with the local and global properties of nonnegative solutions for semilinear heat equation \(u_t-\Delta u=u^p+M|\nabla u|^q\) u t - Δ u = u p + M | u | q in \(\Omega \times I\subset \mathbb {R}^N\times \mathbb {R}\) Ω × I R N × R , where \(M>0\) M > 0 , and \(p,q>1\) p , q > 1 . We first establish the local pointwise gradient estimates when q is subcritical, critical and supercritical with respect to p. With these estimates, we can prove the parabolic Liouville-type theorems for time-decreasing ancient solutions. Next, we use Gidas–Spruck type integral methods to prove the Liouville-type theorem for the entire solutions when q is critical. Finally, as an application of the Liouville-type theorem, we use the doubling lemma to derive universal priori estimates for local solutions of parabolic equations with general nonlinearities. Our approach relies on a parabolic differential inequality containing a suitable auxiliary function rather than Keller–Osserman type inequality, which allows us to generalize and extend the partial results of the elliptic equation (Bidaut-Véron et al. in Math. Ann. 378(1–2):13–56, 2020) to the parabolic case.