The well-posedness problem of an anisotropic porous medium equation with a convection term

Abstract The initial boundary value problem of an anisotropic porous medium equation is considered in this paper. The existence of a weak solution is proved by the monotone convergent method. By showing that ∇ u ∈ L ∞ ( 0 , T ; L loc 2 ( Ω ) ) $\nabla u\in L^{\infty}(0,T; L^{2}_{\mathrm{loc}}(\Omega...

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Main Authors: Yuan Zhi, Huashui Zhan
Format: Article
Language:English
Published: SpringerOpen 2022-08-01
Series:Journal of Inequalities and Applications
Subjects:
Online Access:https://doi.org/10.1186/s13660-022-02847-4
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author Yuan Zhi
Huashui Zhan
author_facet Yuan Zhi
Huashui Zhan
author_sort Yuan Zhi
collection DOAJ
description Abstract The initial boundary value problem of an anisotropic porous medium equation is considered in this paper. The existence of a weak solution is proved by the monotone convergent method. By showing that ∇ u ∈ L ∞ ( 0 , T ; L loc 2 ( Ω ) ) $\nabla u\in L^{\infty}(0,T; L^{2}_{\mathrm{loc}}(\Omega ))$ , according to different boundary value conditions, some stability theorems of weak solutions are obtained. The unusual thing is that the partial boundary value condition is based on a submanifold Σ of ∂ Ω × ( 0 , T ) $\partial \Omega \times (0,T)$ and, in some special cases, Σ = { ( x , t ) ∈ ∂ Ω × ( 0 , T ) : ∏ a i ( x , t ) > 0 } $\Sigma = \{(x,t)\in \partial \Omega \times (0,T): \prod a_{i}(x,t)>0 \}$ .
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spelling doaj.art-e0add740646c40038728afdbd45143592022-12-22T01:35:39ZengSpringerOpenJournal of Inequalities and Applications1029-242X2022-08-012022112210.1186/s13660-022-02847-4The well-posedness problem of an anisotropic porous medium equation with a convection termYuan Zhi0Huashui Zhan1School of Sciences, Jimei UniversitySchool of Applied Mathematics, Xiamen University of TechnologyAbstract The initial boundary value problem of an anisotropic porous medium equation is considered in this paper. The existence of a weak solution is proved by the monotone convergent method. By showing that ∇ u ∈ L ∞ ( 0 , T ; L loc 2 ( Ω ) ) $\nabla u\in L^{\infty}(0,T; L^{2}_{\mathrm{loc}}(\Omega ))$ , according to different boundary value conditions, some stability theorems of weak solutions are obtained. The unusual thing is that the partial boundary value condition is based on a submanifold Σ of ∂ Ω × ( 0 , T ) $\partial \Omega \times (0,T)$ and, in some special cases, Σ = { ( x , t ) ∈ ∂ Ω × ( 0 , T ) : ∏ a i ( x , t ) > 0 } $\Sigma = \{(x,t)\in \partial \Omega \times (0,T): \prod a_{i}(x,t)>0 \}$ .https://doi.org/10.1186/s13660-022-02847-4Anisotropic porous medium equationStability theoremPartial boundary conditionSubmanifold
spellingShingle Yuan Zhi
Huashui Zhan
The well-posedness problem of an anisotropic porous medium equation with a convection term
Journal of Inequalities and Applications
Anisotropic porous medium equation
Stability theorem
Partial boundary condition
Submanifold
title The well-posedness problem of an anisotropic porous medium equation with a convection term
title_full The well-posedness problem of an anisotropic porous medium equation with a convection term
title_fullStr The well-posedness problem of an anisotropic porous medium equation with a convection term
title_full_unstemmed The well-posedness problem of an anisotropic porous medium equation with a convection term
title_short The well-posedness problem of an anisotropic porous medium equation with a convection term
title_sort well posedness problem of an anisotropic porous medium equation with a convection term
topic Anisotropic porous medium equation
Stability theorem
Partial boundary condition
Submanifold
url https://doi.org/10.1186/s13660-022-02847-4
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