A representation formula for the voltage perturbations caused by diametrically small conductivity inhomogeneities. Proof of uniform validity
Hoai-Minh Nguyen, Michael S. Vogelius (2009)
Annales de l'I.H.P. Analyse non linéaire
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Hoai-Minh Nguyen, Michael S. Vogelius (2009)
Annales de l'I.H.P. Analyse non linéaire
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Lieberman, Gary M. (2007)
Boundary Value Problems [electronic only]
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Yves Capdeboscq, Michael S. Vogelius (2003)
ESAIM: Mathematical Modelling and Numerical Analysis - Modélisation Mathématique et Analyse Numérique
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We establish an asymptotic representation formula for the steady state voltage perturbations caused by low volume fraction internal conductivity inhomogeneities. This formula generalizes and unifies earlier formulas derived for special geometries and distributions of inhomogeneities.
Antonio Gaudiello, Rejeb Hadiji (2009)
Annales de l'I.H.P. Analyse non linéaire
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Nicaise, Serge, Zaïr, Ouahiba (2003)
Portugaliae Mathematica. Nova Série
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Bouziani, Abdelfatah (2004)
International Journal of Mathematics and Mathematical Sciences
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Laurent Bourgeois (2010)
ESAIM: Mathematical Modelling and Numerical Analysis
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This paper is devoted to a conditional stability estimate related to the ill-posed Cauchy problems for the Laplace's equation in domains with boundary. It is an extension of an earlier result of [Phung, (2003) 621–635] for domains of class . Our estimate is established by using a Carleman estimate near the boundary in which the exponential weight depends on the distance function to the boundary. Furthermore, we prove that this stability...
Rabello, Tania Nunes, de Campos Vieira, Maria Cristina (2005)
Journal of Inequalities and Applications [electronic only]
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Stanislav N. Antontsev, Gérard Gagneux, Robert Luce, Guy Vallet (2006)
ESAIM: Mathematical Modelling and Numerical Analysis
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This work deals with the study of some stratigraphic models for the formation of geological basins under a maximal erosion rate constrain. It leads to introduce differential inclusions of degenerated hyperbolic-parabolic type , where is the maximal monotonous graph of the Heaviside function and is a given non-negative function. Firstly, we present the new and realistic models and an original mathematical formulation, taking into account the rate constraint in the conservation law,...