Asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition

We study non-negative solutions of the porous medium equation with a source and a nonlinear flux boundary condition, ut = (um)xx + up in (0, ∞) × (0, T); -(um)x (0, t) = uq(0, t) for t ∈ (0, T); u(x, 0) = u0(x) in (0, ∞), where m > 1, p, q > 0 are parameters. For every fixed m we prove...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: De Pablo, A., Quirós, F., Rossi, J.D.
Formato: JOUR
Materias:
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_02724960_v67_n1_p69_DePablo
Aporte de:
id todo:paper_02724960_v67_n1_p69_DePablo
record_format dspace
spelling todo:paper_02724960_v67_n1_p69_DePablo2023-10-03T15:15:15Z Asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition De Pablo, A. Quirós, F. Rossi, J.D. Blow up Nonlinear boundary condition Porous medium equation Boundary conditions Boundary value problems Curve fitting Integration Mathematical models Porous materials Theorem proving Thermal conductivity Asymptotic simplification Blow up solution Fujita curve Nonlinear boundary condition Porous medium equation Reaction diffusion problem Asymptotic stability We study non-negative solutions of the porous medium equation with a source and a nonlinear flux boundary condition, ut = (um)xx + up in (0, ∞) × (0, T); -(um)x (0, t) = uq(0, t) for t ∈ (0, T); u(x, 0) = u0(x) in (0, ∞), where m > 1, p, q > 0 are parameters. For every fixed m we prove that there are two critical curves in the (p, q)-plane: (i) the critical existence curve, separating the region where every solution is global from the region where there exist blowing-up solutions, and (ii) the Fujita curve, separating a region of parameters in which all solutions blow up from a region where both global in time solutions and blowing-up solutions exist. In the case of blow up we find the blow-up rates, the blow-up sets and the blow-up profiles, showing that there is a phenomenon of asymptotic simplification. If 2q < p + m the asymptotics are governed by the source term. On the other hand, if 2q > p + m the evolution close to blow up is ruled by the boundary flux. If 2q = p + m both terms are of the same order. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_02724960_v67_n1_p69_DePablo
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Blow up
Nonlinear boundary condition
Porous medium equation
Boundary conditions
Boundary value problems
Curve fitting
Integration
Mathematical models
Porous materials
Theorem proving
Thermal conductivity
Asymptotic simplification
Blow up solution
Fujita curve
Nonlinear boundary condition
Porous medium equation
Reaction diffusion problem
Asymptotic stability
spellingShingle Blow up
Nonlinear boundary condition
Porous medium equation
Boundary conditions
Boundary value problems
Curve fitting
Integration
Mathematical models
Porous materials
Theorem proving
Thermal conductivity
Asymptotic simplification
Blow up solution
Fujita curve
Nonlinear boundary condition
Porous medium equation
Reaction diffusion problem
Asymptotic stability
De Pablo, A.
Quirós, F.
Rossi, J.D.
Asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition
topic_facet Blow up
Nonlinear boundary condition
Porous medium equation
Boundary conditions
Boundary value problems
Curve fitting
Integration
Mathematical models
Porous materials
Theorem proving
Thermal conductivity
Asymptotic simplification
Blow up solution
Fujita curve
Nonlinear boundary condition
Porous medium equation
Reaction diffusion problem
Asymptotic stability
description We study non-negative solutions of the porous medium equation with a source and a nonlinear flux boundary condition, ut = (um)xx + up in (0, ∞) × (0, T); -(um)x (0, t) = uq(0, t) for t ∈ (0, T); u(x, 0) = u0(x) in (0, ∞), where m > 1, p, q > 0 are parameters. For every fixed m we prove that there are two critical curves in the (p, q)-plane: (i) the critical existence curve, separating the region where every solution is global from the region where there exist blowing-up solutions, and (ii) the Fujita curve, separating a region of parameters in which all solutions blow up from a region where both global in time solutions and blowing-up solutions exist. In the case of blow up we find the blow-up rates, the blow-up sets and the blow-up profiles, showing that there is a phenomenon of asymptotic simplification. If 2q < p + m the asymptotics are governed by the source term. On the other hand, if 2q > p + m the evolution close to blow up is ruled by the boundary flux. If 2q = p + m both terms are of the same order.
format JOUR
author De Pablo, A.
Quirós, F.
Rossi, J.D.
author_facet De Pablo, A.
Quirós, F.
Rossi, J.D.
author_sort De Pablo, A.
title Asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition
title_short Asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition
title_full Asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition
title_fullStr Asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition
title_full_unstemmed Asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition
title_sort asymptotic simplification for a reaction-diffusion problem with a nonlinear boundary condition
url http://hdl.handle.net/20.500.12110/paper_02724960_v67_n1_p69_DePablo
work_keys_str_mv AT depabloa asymptoticsimplificationforareactiondiffusionproblemwithanonlinearboundarycondition
AT quirosf asymptoticsimplificationforareactiondiffusionproblemwithanonlinearboundarycondition
AT rossijd asymptoticsimplificationforareactiondiffusionproblemwithanonlinearboundarycondition
_version_ 1807320651057332224