Uniqueness for cross-diffusion systems issuing from seawater intrusion problems
We consider a model mixing sharp and diffuse interface approaches for seawater intrusion phenomenons in confined and unconfined aquifers. More precisely, a phase field model is introduced in the boundary conditions on the virtual sharp interfaces. We thus include in the model the existence of di...
Main Authors: | , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Texas State University
2017-10-01
|
Series: | Electronic Journal of Differential Equations |
Subjects: | |
Online Access: | http://ejde.math.txstate.edu/Volumes/2017/256/abstr.html |
id |
doaj-52553f7c8f0d48abad24fa0abaa88368 |
---|---|
record_format |
Article |
spelling |
doaj-52553f7c8f0d48abad24fa0abaa883682020-11-24T23:47:17ZengTexas State UniversityElectronic Journal of Differential Equations1072-66912017-10-012017256,122Uniqueness for cross-diffusion systems issuing from seawater intrusion problemsCatherine Choquet0Ji Li1Carole Rosier2 Univ. de La Rochelle, La Rochelle, France Chongqing Technology and Business Univ., China ULCO, LMPA J. Liouville, Calais, France We consider a model mixing sharp and diffuse interface approaches for seawater intrusion phenomenons in confined and unconfined aquifers. More precisely, a phase field model is introduced in the boundary conditions on the virtual sharp interfaces. We thus include in the model the existence of diffuse transition zones but we preserve the simplified structure allowing front tracking. The three-dimensional problem then reduces to a two-dimensional model involving a strongly coupled system of partial differential equations of parabolic and elliptic type describing the evolution of the depth of the interface between salt- and freshwater and the evolution of the freshwater hydraulic head. Assuming a low hydraulic conductivity inside the aquifer, we prove the uniqueness of a weak solution for the model completed with initial and boundary conditions. Thanks to a generalization of a Meyer's regularity result, we establish that the gradient of the solution belongs to the space $L^r$, r>2. This additional regularity combined with the Gagliardo-Nirenberg inequality for r=4 allows to handle the nonlinearity of the system in the proof of uniqueness.http://ejde.math.txstate.edu/Volumes/2017/256/abstr.htmlUniquenesscross-diffusion systemnonlinear parabolic equationsseawater intrusion |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Catherine Choquet Ji Li Carole Rosier |
spellingShingle |
Catherine Choquet Ji Li Carole Rosier Uniqueness for cross-diffusion systems issuing from seawater intrusion problems Electronic Journal of Differential Equations Uniqueness cross-diffusion system nonlinear parabolic equations seawater intrusion |
author_facet |
Catherine Choquet Ji Li Carole Rosier |
author_sort |
Catherine Choquet |
title |
Uniqueness for cross-diffusion systems issuing from seawater intrusion problems |
title_short |
Uniqueness for cross-diffusion systems issuing from seawater intrusion problems |
title_full |
Uniqueness for cross-diffusion systems issuing from seawater intrusion problems |
title_fullStr |
Uniqueness for cross-diffusion systems issuing from seawater intrusion problems |
title_full_unstemmed |
Uniqueness for cross-diffusion systems issuing from seawater intrusion problems |
title_sort |
uniqueness for cross-diffusion systems issuing from seawater intrusion problems |
publisher |
Texas State University |
series |
Electronic Journal of Differential Equations |
issn |
1072-6691 |
publishDate |
2017-10-01 |
description |
We consider a model mixing sharp and diffuse interface approaches
for seawater intrusion phenomenons in confined and unconfined aquifers.
More precisely, a phase field model is introduced in the boundary conditions
on the virtual sharp interfaces.
We thus include in the model the existence of diffuse transition zones but
we preserve the simplified structure allowing front tracking.
The three-dimensional problem then reduces to a two-dimensional
model involving a strongly coupled system of partial differential equations
of parabolic and elliptic type describing the evolution of the depth of the
interface between salt- and freshwater and the evolution of the freshwater
hydraulic head.
Assuming a low hydraulic conductivity inside the aquifer, we prove the
uniqueness of a weak solution for the model completed with initial and boundary
conditions. Thanks to a generalization of a Meyer's regularity result,
we establish that the gradient of the solution belongs to the space $L^r$,
r>2. This additional regularity combined with the Gagliardo-Nirenberg
inequality for r=4 allows to handle the nonlinearity of the system in
the proof of uniqueness. |
topic |
Uniqueness cross-diffusion system nonlinear parabolic equations seawater intrusion |
url |
http://ejde.math.txstate.edu/Volumes/2017/256/abstr.html |
work_keys_str_mv |
AT catherinechoquet uniquenessforcrossdiffusionsystemsissuingfromseawaterintrusionproblems AT jili uniquenessforcrossdiffusionsystemsissuingfromseawaterintrusionproblems AT carolerosier uniquenessforcrossdiffusionsystemsissuingfromseawaterintrusionproblems |
_version_ |
1725490543145779200 |