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...

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Main Authors: Catherine Choquet, Ji Li, Carole Rosier
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
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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
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