Abstract:We consider a time-dependent model for the diffusion of a substance through an incompressible fluid in a perforated domain Ω , Ω ⊂ Ω ⊂ R n with n = 3, 4. The fluid flows in a domain containing a periodical set of "obstacles" (Ω∖Ω ) placed along an inner (n − 1)-dimensional manifold Σ ⊂ Ω. The size of the obstacles is much smaller than the size of the characteristic period . An advection term appears in the partial differential equation linking the fluid velocity with the concentration, while we assume a nonlin… Show more
“…The technique of matched asymptotic expansions, which follows from that in [9,10] and [12], with the suitable modifications, leads us to the homogenized problems listed below:…”
Section: The Homogenized Problems and The Local Problemsmentioning
confidence: 99%
“…Let us refer to [5,6] and references therein for rapidly alternating Dirichlet-Steklov boundary conditions and [11,18,28] for further references and possible applications in the framework of Geophysics and Winkler beds (foundations). See [9][10][11][12][13][14][15] and [32] for an extensive and updated bibliography on different boundary homogenization problems with Robin-type boundary conditions. Finally, we also mention the first works [16] and [19] where different strange terms in the homogenization of volume perforated media with nonlinear-Robin boundary conditions have been introduced.…”
We consider a homogenization problem for the Laplace operator posed in a bounded domain of the upper half-space, a part of its boundary being in contact with the plane $$\{x_3=0\}$$
{
x
3
=
0
}
. On this part, the boundary conditions alternate from Neumann to nonlinear-Robin, being of Dirichlet type outside. The nonlinear-Robin boundary conditions are imposed on small regions periodically placed along the plane and contain a Robin parameter that can be very large. We provide all the possible homogenized problems, depending on the relations between the three parameters: period $$\varepsilon $$
ε
, size of the small regions $$r_\varepsilon $$
r
ε
and Robin parameter $$\beta (\varepsilon )$$
β
(
ε
)
. In particular, we address the convergence, as $$\varepsilon $$
ε
tends to zero, of the solutions for the critical size of the small regions $$r_\varepsilon =O(\varepsilon ^{ 2})$$
r
ε
=
O
(
ε
2
)
. For certain $$\beta (\varepsilon )$$
β
(
ε
)
, a nonlinear capacity term arises in the strange term which depends on the macroscopic variable and allows us to extend the usual capacity definition to semilinear boundary conditions.
“…The technique of matched asymptotic expansions, which follows from that in [9,10] and [12], with the suitable modifications, leads us to the homogenized problems listed below:…”
Section: The Homogenized Problems and The Local Problemsmentioning
confidence: 99%
“…Let us refer to [5,6] and references therein for rapidly alternating Dirichlet-Steklov boundary conditions and [11,18,28] for further references and possible applications in the framework of Geophysics and Winkler beds (foundations). See [9][10][11][12][13][14][15] and [32] for an extensive and updated bibliography on different boundary homogenization problems with Robin-type boundary conditions. Finally, we also mention the first works [16] and [19] where different strange terms in the homogenization of volume perforated media with nonlinear-Robin boundary conditions have been introduced.…”
We consider a homogenization problem for the Laplace operator posed in a bounded domain of the upper half-space, a part of its boundary being in contact with the plane $$\{x_3=0\}$$
{
x
3
=
0
}
. On this part, the boundary conditions alternate from Neumann to nonlinear-Robin, being of Dirichlet type outside. The nonlinear-Robin boundary conditions are imposed on small regions periodically placed along the plane and contain a Robin parameter that can be very large. We provide all the possible homogenized problems, depending on the relations between the three parameters: period $$\varepsilon $$
ε
, size of the small regions $$r_\varepsilon $$
r
ε
and Robin parameter $$\beta (\varepsilon )$$
β
(
ε
)
. In particular, we address the convergence, as $$\varepsilon $$
ε
tends to zero, of the solutions for the critical size of the small regions $$r_\varepsilon =O(\varepsilon ^{ 2})$$
r
ε
=
O
(
ε
2
)
. For certain $$\beta (\varepsilon )$$
β
(
ε
)
, a nonlinear capacity term arises in the strange term which depends on the macroscopic variable and allows us to extend the usual capacity definition to semilinear boundary conditions.
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