<?xml version="1.0" encoding="utf-8"?>
<!DOCTYPE raweb PUBLIC "-//INRIA//DTD " "raweb2.dtd">
<raweb xmlns:xlink="http://www.w3.org/1999/xlink" xml:lang="en" year="2012">
  <identification id="magique-3d" isproject="true">
    <shortname>MAGIQUE-3D</shortname>
    <projectName>Advanced 3D Numerical Modeling in Geophysics</projectName>
    <theme-de-recherche>Observation and Modeling for Environmental Sciences</theme-de-recherche>
    <domaine-de-recherche>Computational Sciences for Biology, Medicine and the Environment</domaine-de-recherche>
    <urlTeam>http://uppa-inria.univ-pau.fr/m3d/</urlTeam>
    <datecreation type="Project-Team">July 01, 2007 </datecreation>
    <structure_exterieure type="Labs">
      <libelle>Laboratoire de mathématiques et de leurs applications (LMAP)</libelle>
    </structure_exterieure>
    <structure_exterieure type="Organism">
      <libelle>CNRS</libelle>
    </structure_exterieure>
    <structure_exterieure type="Organism">
      <libelle>Université de Pau et des Pays de l'Adour</libelle>
    </structure_exterieure>
    <UR name="Bordeaux"/>
    <keywords>
      <term>Waves</term>
      <term>Numerical Methods</term>
      <term>Inverse Problem</term>
      <term>Geophysics</term>
      <term>High Performance Computing</term>
      <term>Scientific Computation</term>
      <term>Finite Elements</term>
      <term>Multiscale Models</term>
      <term>Fluid-Structure Interaction</term>
    </keywords>
  </identification>
  <team id="uid1">
    <person key="magique-3d-2006-idm245547898016">
      <firstname>Hélène</firstname>
      <lastname>Barucq</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>Chercheur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Team Leader, Senior Researcher, Inria</moreinfo>
      <hdr>oui</hdr>
    </person>
    <person key="iparla-2006-idm118158492848">
      <firstname>Josy</firstname>
      <lastname>Baron</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>Assistant</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria</moreinfo>
    </person>
    <person key="magique-3d-2006-idm245547891872">
      <firstname>Mohamed</firstname>
      <lastname>Amara</lastname>
      <affiliation>UnivFr</affiliation>
      <categoryPro>Enseignant</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Professor, University of Pau and Pays de l'Adour, President of UPPA, part-time 20%)</moreinfo>
      <hdr>oui</hdr>
    </person>
    <person key="magique-3d-2006-idm245547889232">
      <firstname>Julien</firstname>
      <lastname>Diaz</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>Chercheur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Junior
Researcher, Inria</moreinfo>
    </person>
    <person key="poems-2006-idm290075532848">
      <firstname>Marc</firstname>
      <lastname>Duruflé</lastname>
      <affiliation>UnivFr</affiliation>
      <categoryPro>Enseignant</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Associate Professor, ENSEIRB-MATMECA</moreinfo>
    </person>
    <person key="magique-3d-2009-idm106187932048">
      <firstname>Taous-Meriem</firstname>
      <lastname>Laleg-Kirati</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>Chercheur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Junior Researcher, Inria, on secondment at KAUST (King Abdullah University of Sciences and Technology), Saudi Arabia since december 2010</moreinfo>
    </person>
    <person key="mc2-2009-idm136144588192">
      <firstname>Victor</firstname>
      <lastname>Péron</lastname>
      <affiliation>UnivFr</affiliation>
      <categoryPro>Enseignant</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Associate Professor, University of Pau and Pays de l'Adour</moreinfo>
    </person>
    <person key="magique-3d-2010-idm149280208352">
      <firstname>Sébastien</firstname>
      <lastname>Tordeux</lastname>
      <affiliation>UnivFr</affiliation>
      <categoryPro>Enseignant</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Associate Professor, Chair of excellence Inria/UPPA, University of Pau and Pays de l'Adour &amp;&amp; Inria</moreinfo>
    </person>
    <person key="magique-3d-2011-idm56653188384">
      <firstname>Julen</firstname>
      <lastname>Alvarez Aramberri</lastname>
      <affiliation>UnivFr</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Bilbao University, since October 2011, till september 2013</moreinfo>
    </person>
    <person key="magique-3d-2011-idm56653182208">
      <firstname>Lionel</firstname>
      <lastname>Boillot</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, CORDI/C Inria - TOTAL,
since May 2011 till december 2014</moreinfo>
    </person>
    <person key="magique-3d-2012-idm163272390048">
      <firstname>Marie</firstname>
      <lastname>Bonnasse Gahot</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, CORDI/C Inria - TOTAL, since October 2012, till October 2015</moreinfo>
    </person>
    <person key="magique-3d-2012-idm163272386944">
      <firstname>Théophile</firstname>
      <lastname>Chaumont Frelet</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, CORDI/C Inria - TOTAL, since October 2012, till October 2015</moreinfo>
    </person>
    <person key="concha-2009-idm183135559424">
      <firstname>Élodie</firstname>
      <lastname>Estecahandy</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, Conseil Régional d'Aquitaine, since November 2010 till October 2013</moreinfo>
    </person>
    <person key="poems-2008-idm380563475520">
      <firstname>Juliette</firstname>
      <lastname>Chabassier</lastname>
      <affiliation>UnivFr</affiliation>
      <categoryPro>PostDoc</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Université de Pau et des Pays de l'Adour, since March 2012 till March 2013</moreinfo>
    </person>
    <person key="apics-2008-idm471168810864">
      <firstname>Yannick</firstname>
      <lastname>Fischer</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PostDoc</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, since December 2011 till November 2012</moreinfo>
    </person>
    <person key="magique-3d-2012-idm163272374384">
      <firstname>Ángel</firstname>
      <lastname>Rodríguez Rozas</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PostDoc</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, Conseil Régional d'Aquitaine, since November 2012, till October 2014</moreinfo>
    </person>
    <person key="magique-3d-2010-idm149280180368">
      <firstname>Emiljana</firstname>
      <lastname>Jorgji</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>Technique</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Associate
Engineer, Inria, since October 2010 till September 2012</moreinfo>
    </person>
    <person key="magique-3d-2011-idm56653163584">
      <firstname>Jérôme</firstname>
      <lastname>Luquel</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, CORDI/C Inria - TOTAL,
since October 2011 till October 2014</moreinfo>
    </person>
    <person key="magique-3d-2011-idm56653160480">
      <firstname>Vanessa</firstname>
      <lastname>Mattesi</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, Conseil Régional d'Aquitaine, since October 2011 till October 2014</moreinfo>
    </person>
    <person key="magique-3d-2012-idm163272361712">
      <firstname>Vincent</firstname>
      <lastname>Popie</lastname>
      <affiliation>EtablissementPrive</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>ONERA, since October 2012 till October 2015</moreinfo>
    </person>
    <person key="magique-3d-2010-idm149280189552">
      <firstname>Florent</firstname>
      <lastname>Ventimiglia</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>PhD</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Inria, CORDI/C Inria - TOTAL,
since November 2010 till November 2013</moreinfo>
    </person>
    <person key="magique-3d-2006-idm245547873264">
      <firstname>Roland</firstname>
      <lastname>Martin</lastname>
      <affiliation>CNRS</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Research
Engineer, CNRS</moreinfo>
      <hdr>oui</hdr>
    </person>
    <person key="magique-3d-2011-idm56654205088">
      <firstname>Abderrahmane</firstname>
      <lastname>Bendali</lastname>
      <affiliation>UnivFr</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Professor, INSA Toulouse</moreinfo>
    </person>
    <person key="magique-3d-2008-idm18158802496">
      <firstname>Chokri</firstname>
      <lastname>Bekkey</lastname>
      <affiliation>UnivEtrangere</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Faculté
des Sciences de Monastir &amp; Laboratoire
d'Ingénierie Mathématique, Ecole Polytechnique de
Tunisie, Assistant Professor (MdC)</moreinfo>
    </person>
    <person key="magique-3d-2006-idm245547847584">
      <firstname>Henri</firstname>
      <lastname>Calandra</lastname>
      <affiliation>EtablissementPrive</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Research Expert Engineer, Total, France</moreinfo>
    </person>
    <person key="magique-3d-2007-idm105910015968">
      <firstname>Bertrand</firstname>
      <lastname>Denel</lastname>
      <affiliation>EtablissementPrive</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Research Engineer, TOTAL, France</moreinfo>
    </person>
    <person key="magique-3d-2006-idm245547839440">
      <firstname>Christian</firstname>
      <lastname>Gout</lastname>
      <affiliation>UnivFr</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Professor, INSA de Rouen</moreinfo>
      <hdr>oui</hdr>
    </person>
    <person key="magique-3d-2006-idm245547842096">
      <firstname>Rabia</firstname>
      <lastname>Djellouli</lastname>
      <affiliation>UnivEtrangere</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Professor, California State University at Northridge, USA</moreinfo>
    </person>
    <person key="magique-3d-2006-idm245547883904">
      <firstname>Dimitri</firstname>
      <lastname>Komatitsch</lastname>
      <affiliation>CNRS</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Senior Researcher</moreinfo>
      <hdr>oui</hdr>
    </person>
    <person key="caiman-2006-idm450347370576">
      <firstname>Stéphane</firstname>
      <lastname>Lanteri</lastname>
      <affiliation>INRIA</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Senior Researcher, Nachos, Inria</moreinfo>
      <hdr>oui</hdr>
    </person>
    <person key="magique-3d-2012-idm163272325952">
      <firstname>David</firstname>
      <lastname>Pardo</lastname>
      <affiliation>UnivEtrangere</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Senior Researcher, University of Basque Country, Spain</moreinfo>
    </person>
    <person key="magique-3d-2012-idm163272322848">
      <firstname>Estelle</firstname>
      <lastname>Piot</lastname>
      <affiliation>EtablissementPrive</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Research Engineer, Onera, France</moreinfo>
    </person>
    <person key="gallium-2006-idm16698279520">
      <firstname>Didier</firstname>
      <lastname>Rémy</lastname>
      <affiliation>EtablissementPrive</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Engineer, SGI, France</moreinfo>
    </person>
    <person key="magique-3d-2007-idm105909996816">
      <firstname>Mounir</firstname>
      <lastname>Tlemcani</lastname>
      <affiliation>UnivEtrangere</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Assistant Professor, University of Oran, Algeria</moreinfo>
    </person>
    <person key="magique-3d-2012-idm163272313536">
      <firstname>Paul</firstname>
      <lastname>Williamson</lastname>
      <affiliation>EtablissementPrive</affiliation>
      <categoryPro>CollaborateurExterieur</categoryPro>
      <research-centre>Bordeaux</research-centre>
      <moreinfo>Research Expert Engineer, Total, France</moreinfo>
    </person>
  </team>
  <presentation id="uid2">
    <bodyTitle>Overall Objectives</bodyTitle>
    <subsection id="uid3" level="1">
      <bodyTitle>General
setting</bodyTitle>
      <p><span class="smallcap" align="left">Magique-3D</span> is a joint project-team between Inria and
the Department of Applied Mathematics (LMA) of the University of Pau, which is associated with CNRS.
Gathering several researchers of different
backgrounds in mathematics
and scientific computing, MAGIQUE-3D team aims at
developing sophisticated modeling tools,
validating them in a rigorous way and applying
them to real cases of geophysical interest. This
project is intrinsically multi-disciplinary and is
strongly related to the regional and national
industrial environment. In particular, we develop
strong collaborations with TOTAL but the topics
studied can lead to applications other than
petroleum engineering. Since it has been created,
MAGIQUE-3D works `Depth Imaging': this topic is related
to modeling of seismic wave propagation in complex
geological structures, taking into account underlying
physical phenomena. It has been defined jointly
by working groups composed of members of
MAGIQUE-3D and of its main industrial partner
TOTAL in order to make sure that actual results of
interest in the context of the oil industry could
be reached. One usually tackles such problems by
adopting two different approaches. The first one consists in defining approximate models that lead to
less expensive numerical methods (for example by
decreasing the number of unknowns by means of an
approximation of the original equations). The second approach is based on
high-performance numerical methods applied to the
full system, which lead to an accurate solution
but implies a high computation cost. Both of these
approaches are considered in the project.</p>
      <p>Reagrding `Advanced modeling in wave
propagation', the team is involved in realistic
numerical simulation of complex three-dimensional
geophysical phenomena and its comparison with real
data recorded in the field.
One of the main issues is the choice of the numerical method, which
implicitly defines the subset of configurations
that can be studied.
Comparisons with recorded seismic data for
real geological cases have been carried out
and then, numerical algorithms have been optimized
and implemented on parallel computers with a large
number of processors and a large memory size,
within the framework of message-passing
programming. We have reached a maximum resolution
in terms of the seismic frequencies that can be
accurately simulated on currently available
supercomputers.</p>
      <p>MAGIQUE-3D works
on the development of optimized software for the
simulation of 3D phenomena in geophysics. The team
tackled this question addressing different and
complementary issues such as the development of
new discretization schemes, the construction of
new boundary conditions used to reduce the size of
the computational domain, the porting of our
software on GPU to speed up their performances.
All the algorithms we have proposed are compatible
with high resolution techniques.
More recently, we have begun to apply our knowledge on
the direct problem to the solution of inverse
problems. It is now a natural goal for the team
since we develop a significant research program
with Total, in particular in the context of the
research program DIP (Depth Imaging Partnership),
where the solution of inverse problems has become
a big challenge for oil industry.</p>
    </subsection>
  </presentation>
  <fondements id="uid4">
    <bodyTitle>Scientific Foundations</bodyTitle>
    <subsection id="uid5" level="1">
      <bodyTitle>Inverse
Problems</bodyTitle>
      <simplelist>
        <li id="uid6">
          <p noindent="true"><b>Inverse scattering problems.</b> The
determination of the shape of an obstacle from
its effects on known acoustic or
electromagnetic waves is an important problem
in many technologies such as sonar, radar,
geophysical exploration, medical imaging and
nondestructive testing. This inverse obstacle
problem (IOP) is difficult to solve, especially
from a numerical viewpoint, because it is
ill-posed and nonlinear <ref xlink:href="#magique-3d-2012-bid0" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>.
Moreover the precision in the reconstruction of
the shape of an obstacle strongly depends on
the quality of the given far-field pattern
(FFP) measurements: the range of the
measurements set and the level of noise in the
data. Indeed, the numerical experiments (for
example  <ref xlink:href="#magique-3d-2012-bid1" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid2" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid3" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid4" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>)
performed in the resonance region, that is, for
a wavelength that is approximately equal to the
diameter of the obstacle, tend to indicate that
in practice, and at least for simple shapes, a
unique and reasonably good solution of the IOP
can be often computed using only one incident
wave and <i>full aperture</i> far-field data
(FFP measured only at a limited range of
angles), as long as the aperture is larger than
<formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>π</mi></math></formula>. For smaller apertures the reconstruction
of the shape of an obstacle becomes more
difficult and nearly impossible for apertures
smaller than <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>π</mi><mo>/</mo><mn>4</mn></mrow></math></formula>.</p>
          <p noindent="true">This plus the fact that
from a mathematical viewpoint the FFP can be
determined on the entire sphere <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>S</mi><mn>1</mn></mrow></math></formula> from its
knowledge on a subset of <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>S</mi><mn>1</mn></mrow></math></formula> because it is an
<i>analytic</i> function, we propose
<ref xlink:href="#magique-3d-2012-bid5" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid6" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> a solution
methodology to extend the range of FFP data when
measured in a limited aperture and not on the
entire sphere <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>S</mi><mn>1</mn></mrow></math></formula>. It is therefore possible to
solve the IOP numerically when only limited
aperture measurements are available.
The objective of <span class="smallcap" align="left">Magique-3D</span> is to extend this work to 3D problems of acoustic scatterin and to tackle the problem of elasto-acoustic scattering.</p>
        </li>
        <li id="uid7">
          <p noindent="true"><b>Depth Imaging in the context of DIP.</b>
The challenge of seismic imaging is to obtain the
best representation of the subsurface from the
solution of the full wave equation that is the
best mathematical model according to the time
reversibility of its solution. The most used
technique of imaging is RTM (Reverse Time
Migration), <ref xlink:href="#magique-3d-2012-bid7" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, which is an iterative
process based on the solution of a collection of
wave equations. The high complexity of the
propagation medium requires the use of advanced
numerical methods, which allows one to solve
several wave equations quickly and accurately. The
research program DIP has been defined by
researchers of <span class="smallcap" align="left">Magique-3D</span> and engineers of <span class="smallcap" align="left">Total</span> jointly. It has been created with the aim of
gathering researchers of Inria, with different
backgrounds and the scientific programm will be
coordinated by <span class="smallcap" align="left">Magique-3D</span>. In this context, <span class="smallcap" align="left">Magique-3D</span> will
contribute by working on the inverse problem and
by continuing to develop new algorithms in order
to improve the RTM.</p>
        </li>
      </simplelist>
    </subsection>
    <subsection id="uid8" level="1">
      <bodyTitle>Modeling</bodyTitle>
      <p noindent="true">The main activities of Magique-3D in modeling
are the derivation and the analysis of
models that are based on mathematical physics
and are suggested by geophysical problems. In
particular, Magique-3D considers equations of
interest for the oil industry and focus on the
development and the analysis of numerical models
which are well-adapted to solve quickly and
accurately problems set in very large or
unbounded domains as it is generally the case in
geophysics.</p>
      <simplelist>
        <li id="uid9">
          <p noindent="true"><b>High-Order Schemes in Space and Time.</b>
Using the full wave equation for migration implies
very high computational burdens, in order to get high
resolution images. Indeed, to improve the accuracy
of the numerical solution, one must considerably
reduce the space step, which is the distance
between two points of the mesh representing the
computational domain. Obviously this results in
increasing the number of unknowns of the discrete
problem. Besides, the time step, whose value fixes
the number of required iterations for solving the
evolution problem, is linked to the space step
through the CFL (Courant-Friedrichs-Levy)
condition. The CFL number defines an upper bound
for the time step in such a way that the smaller
the space step is, the higher the numbers of
iterations (and of multiplications by the
stiffness matrix) will be. The method that we
proposed in <ref xlink:href="#magique-3d-2012-bid8" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>
allows for the use of local time-step, adapted to
the various sizes of the cells and we recently
extended it to deal with
<formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>p</mi></math></formula>-adaptivity  <ref xlink:href="#magique-3d-2012-bid9" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>. However, this
method can not yet handle dissipation terms, which
prevents us for using absorbing boundary
conditions or Perfectly Matched Layers (PML). To overcome this difficulty, we
will first tackle the problem to used the modified
equation technique  <ref xlink:href="#magique-3d-2012-bid10" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid11" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid12" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> with dissipation terms, which is
still an open problem.</p>
          <p noindent="true">We are also considering an alternative
approach to obtain high-order schemes. The main idea
is to apply first the time discretization
thanks to the modified equation technique and
after to consider the space discretization. Our
approach involves <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>p</mi></math></formula>-harmonic operators, which
can not be discretized by classical finite
elements. For the discretization of the
biharmonic operator in an homogeneous acoustic medium,
both C1 finite elements (such as the Hermite ones)
and Discontinuous Galerkin Finite Elements (DGFE)
can be used while in a discontinuous medium, or
for higher-order operators, DGFE should be
preferred  <ref xlink:href="#magique-3d-2012-bid13" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>. This new method seems to be
well-adapted to <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>p</mi></math></formula>-adaptivity. Therefore, we now
want to couple it to our local time-stepping
method in order to deal with <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>h</mi><mi>p</mi></mrow></math></formula>-adaptivity both
in space and in time. We will then carry out theoretical and numerical
comparisons between this technique and the
classical modified equation scheme.</p>
          <p noindent="true">Once we have performant <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>h</mi><mi>p</mi></mrow></math></formula>-adaptive techniques,
it will be necessary to obtain
error-estimators. Since we consider huge domain
and complex topography, the remeshing of the
domain at each time-step is impossible. One
solution would be to remesh the domain for instance
each 100 time steps, but this could also hamper
the efficiency of the computation. Another idea is
to consider only <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>p</mi></math></formula> adaptivity, since in
this case there is no need to remesh the domain.</p>
        </li>
        <li id="uid10">
          <p noindent="true"><b>Mixed hybrid finite element methods for the wave equation.</b>
The new mixed-hybrid-like method for the solution
of Helmholtz problems at high frequency we have
built enjoys the three following important
properties: (1) unlike classical mixed and hybrid
methods, the method we proposed is not subjected
to an inf-sup condition. Therefore, it does not
involve numerical instabilities like the ones that
have been observed for the DGM method proposed by
Farhat and his collaborators <ref xlink:href="#magique-3d-2012-bid14" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid15" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>. We can thus consider a larger class of
discretization spaces both for the primal and the
dual variables. Hence we can use unstructured
meshes, which is not possible with DGM method (2)
the method requires one to solve Helmholtz
problems which are set inside the elements of the
mesh and are solved in parallel(3) the method
requires to solve a system whose unknowns are
Lagrange multipliers defined at the interfaces of
the elements of the mesh and, unlike a DGM, the
system is hermitian and positive definite. Hence
we can use existing numerical methods such as the
gradient conjugate method. We intend to continue
to work on this subject and our objectives can be
described following three tasks: (1) Follow the
numerical comparison of performances of the new
methods with the ones of DGM. We aim at
considering high order elements such as R16-4,
R32-8, ...; (2)Evaluate the performance of the
method in case of unstructured meshes. This
analysis is very important from a practical point
of view but also because it has been observed that
the DGM deteriorates significantly when using
unstructured meshes; (3) Extend the method to the
3D case. This is the ultimate objective of this
work since we will then be able to consider
applications.</p>
          <p noindent="true">Obviously the study we propose will contain a
mathematical analysis of the method we
propose. The analysis will be done in the same
time and we aim at establishing a priori and a
posteriori estimates, the last being very
important in order to adopt a solution strategy based on
adaptative meshes.</p>
        </li>
        <li id="uid11">
          <p noindent="true"><b>Boundary conditions.</b> The
construction of efficient absorbing conditions
is very important for solving wave equations,
which are generally set in unbounded or very
large domains. The efficiency of the conditions
depends on the type of waves which are absorbed.
Classical conditions absorb propagating waves
but recently new conditions have been derived
for both propagating and evanescent waves in the
case of flat boundaries. MAGIQUE-3D would like
to develop new absorbing boundary conditions
whose derivation is based on the full
factorization of the wave equation using
pseudodifferential calculus. By this way, we can
take the complete propagation phenomenon into
account which means that the boundary condition
takes propagating, grazing and evanescent waves
into account, and then the absorption is
optimized. Moreover our approach can be applied
to arbitrarily-shaped regular surfaces.</p>
          <p noindent="true">We intend to work on the development of
interface conditions that can be used to model
rough interfaces. One approach, already applied
in electromagnetism  <ref xlink:href="#magique-3d-2012-bid16" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, consists in
using homogenization methods which describes the
rough surface by an equivalent transmission
condition. We propose to apply it to the case of
elastodynamic equations written as a first-order
system. In particular, it would be very
interesting to investigate if the rigorous
techniques that have been used
in  <ref xlink:href="#magique-3d-2012-bid17" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid18" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> can be applied to the
theory of elasticity. This type of
investigations could be a way for MAGIQUE-3D to
consider medical applications where rough
interfaces are often involved. Indeed, we would
like to work on the modeling and the numerical
simulation of ultrasonic propagation and its
interaction with partially contacting
interfaces, for instance bone/titanium in the
context of an application to dentures, in
collaboration with G. Haiat (University of Paris
7).</p>
        </li>
        <li id="uid12">
          <p noindent="true"><b>Asymptotic modeling</b>.</p>
          <p>In the context of wave propagation problems, we
are investigating physical problems which
involves multiple scales. Due to the presence of
boundary layers (and/or thin layers, rough
interfaces, geometric singularities), the direct
numerical simulation (DNS) of these phenomenas
involves a large numbers of degrees of freedom
and high performance computing is required. The
aim of this work is to develop credible
alternatives to the DNS approach.
Performing a multi-scale asymptotic analysis, we derive approximate models whose solution can be computed for a low computational cost. We study these approximate models mathematically (well-posedness, uniform error estimates) and numerically (we compare the solution of these approximate models to the solution of the initial model computed with high performance computating).</p>
          <p>We are mostly interested in the following problems.</p>
          <simplelist>
            <li id="uid13">
              <p noindent="true">Eddy current modeling in the context of electrothermic applications for the design of electromagnetic devices in collaboration with laboratories Ampère, Laplace, Inria Team MC2, IRMAR, and F.R.S.-FNRS;</p>
            </li>
            <li id="uid14">
              <p noindent="true">ultrasonic wave propagation through bone-titanium media in medicine in collaboration with Inria Team MC2, and MSME;</p>
            </li>
            <li id="uid15">
              <p noindent="true">asymptotic modeling of multi perforate plates in turbo reactors in collaboration with Cerfacs, INSA-Toulouse, Onera and Snecma in the framework of the ANR APAM.</p>
            </li>
          </simplelist>
        </li>
      </simplelist>
    </subsection>
    <subsection id="uid16" level="1">
      <bodyTitle>High Performance methods for solving
wave equations</bodyTitle>
      <p>Seismic Imaging of realistic 3D complex elastodynamic media does not only require advanced mathematical methods but also High Performing Computing (HPC) technologies, both from a software and hardware point of view. In the framework of our collaboration with Total, we are optimizing our algorithms, based on Discontinuous Galerkin methods, in the following directions.</p>
      <simplelist>
        <li id="uid17">
          <p noindent="true"><b>Minimizing the communications between each processor.</b> One of the main advantages of Discontinuous Galerkin methods is that most of the calculus can be performed locally on each element of the mesh. The communications are ensured by the computations of fluxes on the faces of the elements. Hence, there are only communications between elements sharing a common face. This represents a considerable gain compared to Continuous Finite Element methods where the communications have to be done between elements sharing a common degree of freedom. However, the communications can still be minimized by judiciously choosing the quantities to be passed from one element to another</p>
        </li>
        <li id="uid18">
          <p noindent="true"><b>Hybrid MPI and OpenMP parallel programming.</b>
Since the communications are one of the main bottlenecks for the implementation of the Discontinuous Galerkin in an HPC framework, it is necessary to avoid these communications between two processors sharing the same RAM. To this aim, the partition of the mesh is not performed at the core level but at the chip level and the parallelization between two cores of the same chip is done using OpenMP while the parallelization between two cores of two different chips is done using MPI.</p>
        </li>
        <li id="uid19">
          <p noindent="true"><b>Porting the code on new architectures.</b> We are now planning to port the code on the new Intel Many Integrated Core Architecture (Intel MIC). The optimization of this code should begin in 2013, in collaboration with Dider Rémy of SGI.</p>
        </li>
      </simplelist>
      <p>We are confident in the fact that the optimizations of the code will allow us
to perform large-scale calculations and inversion of geophysical data for models and distributed data volumes with a resolution impossible to reach in the past.</p>
    </subsection>
  </fondements>
  <domaine id="uid20">
    <bodyTitle>Application Domains</bodyTitle>
    <subsection id="uid21" level="1">
      <bodyTitle>Seismic Imaging</bodyTitle>
      <p>The main objective of modern seismic processing
is to find the best representation of the
subsurface that can fit the data recorded during
the seismic acquisition survey. In this context,
the seismic wave equation is the most
appropriate mathematical model. Numerous
research programs and related publications have
been devoted to this equation. An acoustic
representation is suitable if the waves
propagate in a fluid. But the subsurface does
not contain fluids only and the acoustic
representation is not sufficient in the general
case. Indeed the acoustic wave equation does not
take some waves into account, for instance shear
waves, turning waves or the multiples that are
generated after several reflections at the
interfaces between the different layers of the
geological model. It is then necessary to
consider a mathematical model that is more
complex and resolution techniques that can model
such waves. The elastic or viscoelastic wave
equations are then reference models, but they
are much more difficult to solve, in particular
in the 3D case. Hence, we need to develop new
high-performance approximation methods.</p>
      <p>Reflection seismics is an indirect measurement
technique that consists in recording echoes
produced by the propagation of a seismic wave in
a geological model. This wave is created
artificially during seismic acquisition surveys.
These echoes (i.e., reflections) are generated
by the heterogeneities of the model. For
instance, if the seismic wave propagates from a
clay layer to sand, one will observe a sharp
reflected signal in the seismic data recorded in
the field. One then talks about reflection
seismics if the wave is reflected at the
interface between the two media, or talks about
seismic refraction if the wave is transmitted
along the interface. The arrival time of the
echo enables one to locate the position of this
transition, and the amplitude of the echo gives
information on some physical parameters of the
two geological media that are in contact. The
first petroleum exploration surveys were
performed at the beginning of the 1920's and for
instance, the Orchard Salt Dome in Texas (USA)
was discovered in 1924 by the seismic-reflection
method.
</p>
    </subsection>
  </domaine>
  <logiciels id="uid22">
    <bodyTitle>Software</bodyTitle>
    <subsection id="uid23" level="1">
      <bodyTitle>Hou10ni</bodyTitle>
      <p>This software, written in FORTRAN 90, simulates
the propagation of acoustic waves in
heterogeneous 2D and 3D media. It is based on an
Interior Penalty Discontinuous Galerkin Method
(IPDGM). The 2D version of the code has been
implemented in the Reverse Time Migration (RTM)
software of <span class="smallcap" align="left">Total</span> in the framework of the Ph.D
thesis of Caroline Baldassari. The 2D code allows
for the use of meshes composed of cells of
various order (<formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>p</mi></math></formula>-adaptivity in space). For the
time discretization, we used the local time
stepping strategy described at
section <ref xlink:href="#uid8" location="intern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, item <b>High-Order Schemes in Space and Time</b> which permits not
only the use of different time-step, but also to
adapt the order of the time-discretization to
the order of each cells (<formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>h</mi><mi>p</mi></mrow></math></formula>-adaptivity in time).</p>
      <p>The main competitors of Hou10ni are codes based
on Finite Differences, Spectral Element Method
or other Discontinuous Galerkin Methods (such as
the ADER schemes). During her Ph.D thesis,
Caroline Baldassari compared the solution
obtained by Hou10ni to the solution obtained by
a Finite Difference Method and by a Spectral
Element Method (SPECFEM). To evaluate the
accuracy of the solutions, we have compared them
to analytical solutions provided by the codes
Gar6more (see below). The results of these
comparisons is: a) that Hou10ni outperforms the
Finite Difference Methods both in terms of
accuracy and of computational burden and b) that
its performances are similar to Spectral Element
Methods. Since Hou10ni allows for the use of
meshes based on tetraedrons, which are more
appropriate to mesh complex topographies, and
for the <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>p</mi></math></formula>-adaptivity, we decided to implement it in the RTM code of <span class="smallcap" align="left">Total</span>. Of course, we also used these comparisons to validate the code.
Now, it remains to compare the performances of Hou10ni to the ADER schemes.</p>
      <p>Recently, we have extended the 2D version of Hou10ni for computing the solution of the harmonic wave equation (Helmholtz). This new version is able to deal with both acoustic and elastodynamic media, but also to model elastoacoustic problems. The surfaces between the different media can be approximated by curved elements. We can use up to <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><msup><mi>P</mi><mn>15</mn></msup></math></formula> elements when dealing with curved elements and element of arbitrary order (with of course a limitation depending on the machine precision) when dealing with non-curved elements.
</p>
    </subsection>
    <subsection id="uid24" level="1">
      <bodyTitle>
        <ref xlink:href="http://web.univ-pau.fr/~jdiaz1/software.html" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">Gar6more3D</ref>
      </bodyTitle>
      <participants>
        <person key="magique-3d-2006-idm245547889232">
          <firstname>Julien</firstname>
          <lastname>Diaz</lastname>
          <moreinfo>correspondant</moreinfo>
        </person>
      </participants>
      <p>This code computes the analytical solution of problems of waves propagation in two layered 3D media such as- acoustic/acoustic- acoustic/elastodynamic- acoustic/porous- porous/porous, based on the Cagniard-de Hoop method.</p>
      <p noindent="true">See also the web page <ref xlink:href="http://web.univ-pau.fr/~jdiaz1/software.html" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>web.<allowbreak/>univ-pau.<allowbreak/>fr/<allowbreak/>~jdiaz1/<allowbreak/>software.<allowbreak/>html</ref>.</p>
      <p>The main objective of this code is to provide
reference solutions in order to validate
numerical codes. They have been already used by
J. Tromp and C. Morency to validate their code
of poroelastic wave propagation  <ref xlink:href="#magique-3d-2012-bid19" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>.
They are freely distributed under a CECILL
licence and can be downloaded on the website
<ref xlink:href="http://web.univ-pau.fr/~jdiaz1/software.html" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>web.<allowbreak/>univ-pau.<allowbreak/>fr/<allowbreak/>~jdiaz1/<allowbreak/>software.<allowbreak/>html</ref>.
As far as we know, the main competitor of this
code is EX2DELDEL ( available on
<ref xlink:href="http://www.spice-rtn.org" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>www.<allowbreak/>spice-rtn.<allowbreak/>org</ref>), but this code only
deals with 2D acoustic or elastic media. Our
codes seem to be the only one able to deal with
bilayered poroelastic media and to handle the
three dimensional cases.</p>
      <simplelist>
        <li id="uid25">
          <p noindent="true">ACM: J.2</p>
        </li>
        <li id="uid26">
          <p noindent="true">AMS: 34B27 35L05 35L15 74F10 74J05</p>
        </li>
        <li id="uid27">
          <p noindent="true">Programming language: Fortran 90</p>
        </li>
      </simplelist>
    </subsection>
  </logiciels>
  <resultats id="uid28">
    <bodyTitle>New Results</bodyTitle>
    <subsection id="uid29" level="1">
      <bodyTitle>Inverse Problems</bodyTitle>
      <subsection id="cid1" level="2">
        <bodyTitle>Reconstruction of an elastic scatterer immersed in a homogeneous fluid</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="magique-3d-2006-idm245547842096">
            <firstname>Rabia</firstname>
            <lastname>Djellouli</lastname>
          </person>
          <person key="concha-2009-idm183135559424">
            <firstname>Élodie</firstname>
            <lastname>Estecahandy</lastname>
          </person>
        </participants>
        <p>The determination of the shape of an obstacle from its effects on known acoustic or electromagnetic waves is an important problem in many technologies such as sonar, radar, geophysical exploration, medical imaging and nondestructive testing. This inverse obstacle problem (IOP) is difficult to solve, especially from a numerical viewpoint, because it is ill-posed and nonlinear. Its investigation requires as a prerequisite the fundamental understanding of the theory for the associated direct scattering problem, and the mastery of the corresponding numerical solution methods.</p>
        <p noindent="true">In this work, we are interested in retrieving the shape of an elastic obstacle from the knowledge of some scattered far-field patterns, and assuming certain characteristics of the surface of the obstacle. The corresponding direct elasto-acoustic scattering problem consists in the scattering of time-harmonic acoustic waves by an elastic obstacle <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><msup><mi>Ω</mi><mi>s</mi></msup></math></formula> embedded in a homogeneous medium <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><msup><mi>Ω</mi><mi>f</mi></msup></math></formula>, that can be formulated as follows:</p>
        <p>
          <formula id-text="1" id="uid30" textype="eqnarray" type="display">
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                    <mrow>
                      <mi>Δ</mi>
                      <mi>p</mi>
                      <mo>+</mo>
                      <mo>(</mo>
                      <msup>
                        <mi>ω</mi>
                        <mn>2</mn>
                      </msup>
                      <mo>/</mo>
                      <msubsup>
                        <mi>c</mi>
                        <mi>f</mi>
                        <mn>2</mn>
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                      <mi>p</mi>
                      <mo>=</mo>
                      <mn>0</mn>
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                      <mspace width="14.22636pt"/>
                      <mspace width="4.pt"/>
                      <mtext>in</mtext>
                      <mspace width="4.pt"/>
                      <msup>
                        <mi>Ω</mi>
                        <mi>f</mi>
                      </msup>
                    </mrow>
                  </mtd>
                </mtr>
                <mtr>
                  <mtd columnalign="right">
                    <mrow>
                      <mi>∇</mi>
                      <mo>·</mo>
                      <mi>σ</mi>
                      <mrow>
                        <mo>(</mo>
                        <mi>u</mi>
                        <mo>)</mo>
                      </mrow>
                      <mo>+</mo>
                      <msup>
                        <mi>ω</mi>
                        <mn>2</mn>
                      </msup>
                      <msub>
                        <mi>ρ</mi>
                        <mi>s</mi>
                      </msub>
                      <mspace width="0.166667em"/>
                      <mi>u</mi>
                      <mo>=</mo>
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                    <mrow>
                      <mspace width="14.22636pt"/>
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                      <mspace width="4.pt"/>
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                        <mi>s</mi>
                      </msup>
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                </mtr>
                <mtr>
                  <mtd columnalign="right">
                    <mrow>
                      <msup>
                        <mi>ω</mi>
                        <mn>2</mn>
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                      <msub>
                        <mi>ρ</mi>
                        <mi>f</mi>
                      </msub>
                      <mi>u</mi>
                      <mo>·</mo>
                      <mi>n</mi>
                      <mo>=</mo>
                      <mi>∂</mi>
                      <mi>p</mi>
                      <mo>/</mo>
                      <mi>∂</mi>
                      <mi>n</mi>
                      <mo>+</mo>
                      <mi>∂</mi>
                      <msup>
                        <mi>e</mi>
                        <mrow>
                          <mi>i</mi>
                          <mspace width="0.166667em"/>
                          <mo>(</mo>
                          <mi>ω</mi>
                          <mo>/</mo>
                          <msub>
                            <mi>c</mi>
                            <mi>f</mi>
                          </msub>
                          <mo>)</mo>
                          <mspace width="0.166667em"/>
                          <mi>x</mi>
                          <mo>·</mo>
                          <mi>d</mi>
                        </mrow>
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                      <mo>/</mo>
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                      <mi>n</mi>
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                    <mrow>
                      <mspace width="14.22636pt"/>
                      <mspace width="4.pt"/>
                      <mtext>on</mtext>
                      <mspace width="4.pt"/>
                      <mi>Γ</mi>
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                <mtr>
                  <mtd columnalign="right">
                    <mrow>
                      <mi>σ</mi>
                      <mrow>
                        <mo>(</mo>
                        <mi>u</mi>
                        <mo>)</mo>
                      </mrow>
                      <mi>n</mi>
                      <mo>=</mo>
                      <mo>-</mo>
                      <mi>p</mi>
                      <mi>n</mi>
                      <mo>-</mo>
                      <msup>
                        <mi>e</mi>
                        <mrow>
                          <mi>i</mi>
                          <mspace width="0.166667em"/>
                          <mo>(</mo>
                          <mi>ω</mi>
                          <mo>/</mo>
                          <msub>
                            <mi>c</mi>
                            <mi>f</mi>
                          </msub>
                          <mo>)</mo>
                          <mspace width="0.166667em"/>
                          <mi>x</mi>
                          <mo>·</mo>
                          <mi>d</mi>
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                      <mi>n</mi>
                    </mrow>
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                  <mtd>
                    <mrow>
                      <mspace width="14.22636pt"/>
                      <mspace width="4.pt"/>
                      <mtext>on</mtext>
                      <mspace width="4.pt"/>
                      <mi>Γ</mi>
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                <mtr>
                  <mtd columnalign="right">
                    <mrow>
                      <munder>
                        <mo movablelimits="true" form="prefix">lim</mo>
                        <mrow>
                          <mi>r</mi>
                          <mo>→</mo>
                          <mo>+</mo>
                          <mi>∞</mi>
                        </mrow>
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                      <mi>r</mi>
                      <mfenced separators="" open="(" close=")">
                        <mi>∂</mi>
                        <mi>p</mi>
                        <mo>/</mo>
                        <mi>∂</mi>
                        <mi>r</mi>
                        <mo>-</mo>
                        <mi>i</mi>
                        <mspace width="0.166667em"/>
                        <mo>(</mo>
                        <mi>ω</mi>
                        <mo>/</mo>
                        <msub>
                          <mi>c</mi>
                          <mi>f</mi>
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                        <mo>)</mo>
                        <mspace width="0.166667em"/>
                        <mi>p</mi>
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                      <mo>=</mo>
                      <mn>0</mn>
                    </mrow>
                  </mtd>
                </mtr>
              </mtable>
            </math>
          </formula>
        </p>
        <p noindent="true">where <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>p</mi></math></formula> is the fluid pressure in <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><msup><mi>Ω</mi><mi>f</mi></msup></math></formula> whereas <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>u</mi></math></formula> is the displacement field in <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><msup><mi>Ω</mi><mi>s</mi></msup></math></formula>, and <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>σ</mi><mo>(</mo><mi>u</mi><mo>)</mo></mrow></math></formula> represents the stress tensor of the elastic material.</p>
        <p noindent="true">This boundary value problem has been investigated mathematically and results pertaining to the existence, uniqueness and regularity can be found in <ref xlink:href="#magique-3d-2012-bid20" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> and the references therein, among others. We propose a solution methodology based on a regularized Newton-type method for solving the IOP. The proposed method is an extension of the regularized Newton algorithm developed for solving the case where only Helmholtz equation is involved, that is the acoustic case by impenetrable scatterers <ref xlink:href="#magique-3d-2012-bid21" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>. The direct elasto-acoustic scattering problem defines an operator <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>F</mi><mo>:</mo><mi>Γ</mi><mo>→</mo><msub><mi>p</mi><mi>∞</mi></msub></mrow></math></formula> which maps the boundary <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>Γ</mi></math></formula> of the scatterer <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><msup><mi>Ω</mi><mi>s</mi></msup></math></formula> onto the far-field pattern <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><msub><mi>p</mi><mi>∞</mi></msub></math></formula>. Hence, given one or several measured far-field patterns <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><msub><mover accent="true"><mi>p</mi><mo>˜</mo></mover><mi>∞</mi></msub><mrow><mo>(</mo><mover accent="true"><mi>x</mi><mo>^</mo></mover><mo>)</mo></mrow></mrow></math></formula>, corresponding to one or several given directions <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>d</mi></math></formula> and wavenumbers <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>k</mi></math></formula>, one can formulate IOPs as follows:</p>
        <p>
          <formula type="display">
            <math xmlns="http://www.w3.org/1998/Math/MathML" mode="display" overflow="scroll">
              <mrow>
                <mspace width="4.pt"/>
                <mtext>Find</mtext>
                <mspace width="4.pt"/>
                <mtext>a</mtext>
                <mspace width="4.pt"/>
                <mtext>shape</mtext>
                <mspace width="0.277778em"/>
                <mi>Γ</mi>
                <mspace width="0.277778em"/>
                <mspace width="4.pt"/>
                <mtext>such</mtext>
                <mspace width="4.pt"/>
                <mtext>that</mtext>
                <mspace width="1.em"/>
                <mi>F</mi>
                <mrow>
                  <mo>(</mo>
                  <mi>Γ</mi>
                  <mo>)</mo>
                </mrow>
                <mrow>
                  <mo>(</mo>
                  <mover accent="true">
                    <mi>x</mi>
                    <mo>^</mo>
                  </mover>
                  <mo>)</mo>
                </mrow>
                <mo>=</mo>
                <msub>
                  <mover accent="true">
                    <mi>p</mi>
                    <mo>˜</mo>
                  </mover>
                  <mi>∞</mi>
                </msub>
                <mrow>
                  <mo>(</mo>
                  <mover accent="true">
                    <mi>x</mi>
                    <mo>^</mo>
                  </mover>
                  <mo>)</mo>
                </mrow>
                <mo>;</mo>
                <mspace width="1.em"/>
                <mover accent="true">
                  <mi>x</mi>
                  <mo>^</mo>
                </mover>
                <mo>∈</mo>
                <msup>
                  <mi>S</mi>
                  <mn>1</mn>
                </msup>
                <mo>.</mo>
              </mrow>
            </math>
          </formula>
        </p>
        <p noindent="true">We propose a solution methodology based on a regularized Newton-type method to solve this inverse obstacle problem.
At each Newton iteration, we solve the forward problem using a finite element solver based on discontinuous Galerkin approximations, and equipped with high-order absorbing boundary conditions. We have first characterized the Fréchet derivatives of the scattered field. They are solution to the same boundary value problem as the direct problem with other transmission conditions. This work has been presented both in FACM11 and in WAVES 2011. A paper has been submitted.</p>
      </subsection>
      <subsection id="cid2" level="2">
        <bodyTitle><formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>h</mi><mi>p</mi></mrow></math></formula>-adaptive inversion of magnetotelluric measurements</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="magique-3d-2011-idm56653188384">
            <firstname>Julen</firstname>
            <lastname>Alvarez Aramberri</lastname>
          </person>
          <person key="magique-3d-2012-idm163272325952">
            <firstname>David</firstname>
            <lastname>Pardo</lastname>
          </person>
        </participants>
        <p>The magnetotelluric (MT) method is a passive electromagnetic (EM) exploration technique that allows to determine the resistivity distribution in the subsurface of the area of interest on scales varying from few meters to hundreds of kilometers. Commercial uses include hydrocarbon (oil and gas) exploration, geothermal exploration, and mining exploration, as well as hydrocarbon and groundwater monitoring. MT measurements are governed by the electromagnetic phenomena, which can be described by Maxwell's equations. We solve those equations by a goal-oriented hp-adaptivity Finite Element Method (FEM).</p>
        <p>In order to estimate the resistivity distribution in the Earth's subsurface, we solve an Inverse Problem. We define a Misfit Function that represents the difference between the measured and computed data for a particular resistivity distribution. By minimizing this misfit function using a gradient based approach with model reduction techniques, and hence solving the inverse problem, we are able to determine the properties of the subsurface materials.
</p>
      </subsection>
    </subsection>
    <subsection id="uid31" level="1">
      <bodyTitle>Modeling</bodyTitle>
      <subsection id="cid3" level="2">
        <bodyTitle>Implementation of a non-reflecting boundary condition on ellipsoidal boundary</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Anne-Gaëlle</firstname>
            <lastname>Saint-Guirons</lastname>
          </person>
          <person key="magique-3d-2010-idm149280208352">
            <firstname>Sébastien</firstname>
            <lastname>Tordeux</lastname>
          </person>
        </participants>
        <p>The modeling of wave propagation problems using finite element methods usually requires the truncation of the
computational domain around the scatterer of interest. Absorbing boundary condition are classically considered in
order to avoid spurious reflections. This year we have implemented and tested an exact condition based on a non local Dirichlet to Neumann operator in the context of the Helmholtz equation posed on an elongated domain.</p>
      </subsection>
      <subsection id="cid4" level="2">
        <bodyTitle>Explicit computation of the electrostatic energy for an elliptical charged disc</bodyTitle>
        <participants>
          <person key="PASUSERID">
            <firstname>Sophie</firstname>
            <lastname>Laurens</lastname>
          </person>
          <person key="magique-3d-2010-idm149280208352">
            <firstname>Sébastien</firstname>
            <lastname>Tordeux</lastname>
          </person>
        </participants>
        <p>In <ref xlink:href="#magique-3d-2012-bid22" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, We have described a method to obtain an explicit expression for the electro-
static energy of a charged elliptical infinitely thin disc. The charge distribution
is assumed to be polynomial. Such explicit values for this energy are fundamen-
tal for assessing the accuracy of boundary element method codes. The main
tools used are an extension of Copson’s method and a diagonalization, given by
Leppington and Levine, of the single-layer potential operator associated with
the electrostatic potential created by a distribution of charges on an elliptical
disc.</p>
      </subsection>
      <subsection id="cid5" level="2">
        <bodyTitle>A new modified equation approach for
solving the wave equation</bodyTitle>
        <participants>
          <person key="PASUSERID">
            <firstname>Cyril</firstname>
            <lastname>Agut</lastname>
          </person>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="magique-3d-2006-idm245547847584">
            <firstname>Henri</firstname>
            <lastname>Calandra</lastname>
          </person>
          <person key="magique-3d-2006-idm245547889232">
            <firstname>Julien</firstname>
            <lastname>Diaz</lastname>
          </person>
          <person key="magique-3d-2010-idm149280189552">
            <firstname>Florent</firstname>
            <lastname>Ventimiglia</lastname>
          </person>
        </participants>
        <p>The new method involving <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mi>p</mi></math></formula>-harmonic operator
described in section <ref xlink:href="#uid8" location="intern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> has been
presented in <ref xlink:href="#magique-3d-2012-bid23" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>.
We have proved the convergence of
the scheme and its stability under a CFL
condition. Numerical results in one, two and three-dimensional configurations show that this
CFL condition is slightly greater than the CFL
condition of the second-order Leap-Frog scheme.</p>
        <p>In the framework of the PhD thesis of Florent Ventimiglia, we are now considering the extension of this technique to the first order formulation of the acoustic and elastodynamic equations. A numerical analysis of performance in 1D indicates that, for a given accuracy, this method requires less storage than the High-Order ADER Schemes for and similar computational costs. We are now implementing this algorithm in 3D in order to confirm this analysis and to assess its performance in an RTM framework on realistic configurations.</p>
      </subsection>
      <subsection id="cid6" level="2">
        <bodyTitle>Stability Analysis of an Interior Penalty
Discontinuous Galerkin Method for the Wave equation </bodyTitle>
        <participants>
          <person key="PASUSERID">
            <firstname>Cyril</firstname>
            <lastname>Agut</lastname>
          </person>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="magique-3d-2006-idm245547889232">
            <firstname>Julien</firstname>
            <lastname>Diaz</lastname>
          </person>
        </participants>
        <p>The Interior Penalty Discontinuous Galerkin
Method  <ref xlink:href="#magique-3d-2012-bid24" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid25" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid26" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> we use in the
IPDGFEM code requires the introduction of a
penalty parameter. Except for regular
quadrilateral or cubic meshes, the optimal value
of this parameter is not explicitely known.
Moreover, the condition number of the resulting
stiffness matrix is an increasing function of this
parameter, but the precise behaviour has not been
explicited neither. We have carried out a
theoretical and numerical study of the pnealization parameter and of the CFL
condition for quadrilateral and cubic meshes, this results have been presented in a paper accepted in M2AN <ref xlink:href="#magique-3d-2012-bid27" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/></p>
      </subsection>
      <subsection id="cid7" level="2">
        <bodyTitle>Higher Order Absorbing Boundary Conditions
for the Wave Equation</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="poems-2008-idm380563475520">
            <firstname>Juliette</firstname>
            <lastname>Chabassier</lastname>
          </person>
          <person key="magique-3d-2006-idm245547889232">
            <firstname>Julien</firstname>
            <lastname>Diaz</lastname>
          </person>
        </participants>
        <p>The numerical simulation of wave propagation is generally performed by truncating the propagation medium and the team works on new ABCs, trying to improve the performance of existing conditions. Following the analysis performed in <ref xlink:href="#magique-3d-2012-bid28" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, we have considered the issue of constructing high-order ABCs for the Helmholtz equation. Now, to derive conditions of order greater than two is really technical. In addition, when the coefficients representing the geological properties of the medium are not regular, the method of construction of ABCs is not completely justified. That is why we turned to the construction of conditions that take into account all the characteristics of the diffraction phenomenon and not only waves that propagate like in the case of standrad ABCs. This is what we call enriched ABCs. A research report is being written, an article should be submitted in 2013.
During 2012, a publication for the acoustic wave equation has been accepted in M3AS <ref xlink:href="#magique-3d-2012-bid28" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> and a second one has been submitted.</p>
      </subsection>
      <subsection id="cid8" level="2">
        <bodyTitle>Multiperforated plates in linear acoustics</bodyTitle>
        <participants>
          <person key="magique-3d-2011-idm56654205088">
            <firstname>Abderrahmane</firstname>
            <lastname>Bendali</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>M'Barek</firstname>
            <lastname>Fares</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Sophie</firstname>
            <lastname>Laurens</lastname>
          </person>
          <person key="magique-3d-2012-idm163272322848">
            <firstname>Estelle</firstname>
            <lastname>Piot</lastname>
          </person>
          <person key="magique-3d-2010-idm149280208352">
            <firstname>Sébastien</firstname>
            <lastname>Tordeux</lastname>
          </person>
        </participants>
        <p>Acoustic engineers use approximate heuristic models to deal with multiperforated plates in liners and in combustion chambers of turbo-engines. These models were suffering from a lack of mathematical justifications and were consequently difficult to improve. Performing an asymptotic analysis (the small parameter is the radius of the perforations), we have justified these models and proposed some improvement. Our theoretical results have been compared to numerical simulations performed at CERFACS (M'Barek Fares) and to acoustical experiments realized at ONERA (Estelle Piot). Two papers have been published in 2012 <ref xlink:href="#magique-3d-2012-bid29" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid30" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>.</p>
      </subsection>
      <subsection id="cid9" level="2">
        <bodyTitle>Performance Assessment of IPDG for the solution of an elasto-acoustic scattering problem</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="magique-3d-2006-idm245547842096">
            <firstname>Rabia</firstname>
            <lastname>Djellouli</lastname>
          </person>
          <person key="concha-2009-idm183135559424">
            <firstname>Élodie</firstname>
            <lastname>Estecahandy</lastname>
          </person>
        </participants>
        <p>We present a solution methodology for the direct elasto-acoustic scattering problem that falls in the category of Discontinuous Galerkin methods. The method distinguishes itself from the existing methods by combining high-order Discontinuous Galerkin approximations, local stabilizations for the coupled problem and the use of curved element edges on the boundaries. We present some numerical results that illustrate the salient features and highlight the performance of the proposed solution methodology on the resonance phenomenon existing in the elastic scatterer for simple geometries such as circles. Moreover, the designed method ensures a convergence order with a gain of two order of magnitude compared to polygonal boundaries, and a potential to address both mid- and high-frequency regimes. These results have been presented to ECCOMAS 2012 <ref xlink:href="#magique-3d-2012-bid31" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> and to two workshops <ref xlink:href="#magique-3d-2012-bid32" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> <ref xlink:href="#magique-3d-2012-bid33" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>.</p>
      </subsection>
      <subsection id="cid10" level="2">
        <bodyTitle>Operator Based Upscaling for Discontinuous Galerkin Methods</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Théophile</firstname>
            <lastname>Chaumont</lastname>
          </person>
          <person key="magique-3d-2006-idm245547889232">
            <firstname>Julien</firstname>
            <lastname>Diaz</lastname>
          </person>
          <person key="magique-3d-2006-idm245547839440">
            <firstname>Christian</firstname>
            <lastname>Gout</lastname>
          </person>
          <person key="mc2-2009-idm136144588192">
            <firstname>Victor</firstname>
            <lastname>Péron</lastname>
          </person>
        </participants>
        <p>Scientists and engineers generally tackle problems
that include multiscale effects and that are thus
difficult to solve numerically. The main
difficulty is to capture both the fine and the
coarse scales to get an accurate numerical
solution. Indeed, the computations are generally
performed by using numerical schemes based on
grids. But the stability and thus the accuracy of
the numerical method depends on the size of the
grid which must be refined drastically in the case
of very fine scales. That implies huge
computational costs and in particular the
limitations of the memory capacity are often
reached. It is thus necessary to use numerical
methods that are able to capture the fine scale
effects with computations on coarse meshes.
Operator-based upscaling is one of them and we
present in <ref xlink:href="#magique-3d-2012-bid34" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> a first
attempt to adapt that technique to a Discontinuous
Galerkin Method (DGM). We consider the Laplace
problem as a benchmark and we compare the
performance of the resulting numerical scheme with
the classical one using Lagrange finite elements.
The comparison involves both an accuracy analysis
and a complexity calculus. This work shows that
there is an interest of combining DGM with
upscaling.</p>
      </subsection>
      <subsection id="cid11" level="2">
        <bodyTitle>Asymptotic Modeling for Elasto-Acoustics</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547889232">
            <firstname>Julien</firstname>
            <lastname>Diaz</lastname>
          </person>
          <person key="mc2-2009-idm136144588192">
            <firstname>Victor</firstname>
            <lastname>Péron</lastname>
          </person>
        </participants>
        <p>We present in <ref xlink:href="#magique-3d-2012-bid35" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/> equivalent conditions and asymptotic models for the diffraction problem of elasto-acoustic waves in a solid medium surrounded by a thin layer of fluid medium. This problem is well suited for the notion of equivalent conditions : since the thickness of the layer is small with respect to the wavelength, the effect of the fluid medium on the solid is as a first approximation local. We derive and validate equivalent conditions up to the third order for the elastic displacement. These conditions approximate the acoustic waves which propagate in the fluid region. This approach leads us to solve only elastic equations. The construction of equivalent conditions is based on a multiscale expansion in power series of the thickness of the layer for the solution of the transmission problem.</p>
        <p>Questions regarding the implementation of the conditions have been addressed carefully. Indeed, the boundary conditions have been integrated without changing the structure of the code Hou10ni.</p>
        <p>This work has been presented in four international conferences and Workshops : Aquitaine-Euskadi Workshop on Applied Mathematics; First Russian-French Conference on Mathematical Geophysics, Mathematical Modeling in Continuum Mechanics and Inverse Problems; Workshop HPC-GA; Twelfth International Conference Zaragoza-Pau on Mathematics.</p>
        <p>A paper with numerical results for the elasto-acoustic problem with a thin layer and a variable thickness is in preparation.</p>
      </subsection>
      <subsection id="cid12" level="2">
        <bodyTitle>Asymptotic modeling in electromagnetism</bodyTitle>
        <participants>
          <person key="PASUSERID">
            <firstname>François</firstname>
            <lastname>Buret</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Monique</firstname>
            <lastname>Dauge</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Patrick</firstname>
            <lastname>Dular</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Laurent</firstname>
            <lastname>Krähenbühl</lastname>
          </person>
          <person key="mc2-2009-idm136144588192">
            <firstname>Victor</firstname>
            <lastname>Péron</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Ronan</firstname>
            <lastname>Perrussel</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Clair</firstname>
            <lastname>Poignard</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Damien</firstname>
            <lastname>Voyer</lastname>
          </person>
        </participants>
        <p>The following results rely on a problematic developed in section <ref xlink:href="#uid8" location="intern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, item <b>Asymptotic modeling</b>.</p>
        <p>In the paper <ref xlink:href="#magique-3d-2012-bid36" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, eddy current problems are addressed in a bidimensional setting where the conducting medium is non-magnetic and has a corner singularity. For any fixed skin depth we show that the flux density is bounded near the corner, unlike the perfect conducting case. Then as the skin depth goes to zero, the first two terms of a multiscale expansion of the magnetic potential are introduced to tackle the magneto-harmonic problem. The heuristics of the method are given and numerical computations illustrate the obtained accuracy.</p>
        <p>In a forthcoming paper, we describe the magnetic potential in the vicinity
of a corner of a conducting body embedded in a dielectric medium in
a bidimensional setting. We make explicit the corner asymptotic
expansion for this potential as the distance to the corner goes to
zero. This expansion involves singular functions and singular
coefficients. We introduce a method for the calculation of the
singular functions near the corner and we provide two methods
to compute the singular coefficients: the method of moments and the method of quasi-dual
singular functions. Estimates for the convergence of both
approximate methods are proven.
We eventually illustrate the theoretical results with
finite element computations. The specific non-standard feature of this problem lies in the
structure of its singular functions: They have the form of series
whose first terms are harmonic polynomials and further terms are
genuine non-smooth functions generated by the piecewise constant zeroth order
term of the operator. This work has been presented in the international conference WCCM 2012.</p>
      </subsection>
      <subsection id="cid13" level="2">
        <bodyTitle>Asymptotic models for penalization methods in porous media</bodyTitle>
        <participants>
          <person key="PASUSERID">
            <firstname>Gilles</firstname>
            <lastname>Carbou</lastname>
          </person>
          <person key="mc2-2009-idm136144588192">
            <firstname>Victor</firstname>
            <lastname>Péron</lastname>
          </person>
        </participants>
        <p>We investigate a Stokes-Brinkman problem with Beavers and Joseph transmission conditions, adapted to a penalization method in porous media. We exhibit a WKB expansion for the solution of the fluid-porous interface problem. The main interest is to derive equivalent models for the penalization method.
We explicit the first terms of the WKB expansion for the flow and the pressure in the subdomains. Each asymptotics of the flow writes as a sum of a tangential boundary layer term plus a standard term in the porous region. From the benefits or these boundary layers, we infer a collection of elementary transmission problems satisfied by the standard parts of the asymptotics for the flow and the pressure. As a consequence of the penalization of the Laplacian operator which applies to the flow in the porous media, a degenerate operator of order zero applies to the elementary velocities appears in the porous region. The main difficulty concern the proof of elliptic regularity up to the interface for the solution of each elementary problem, since exotic conditions for the flow and the pressure appears along the interface. Our strategy consists to adapt a proof of elliptic regularity for the solution of a Darcy problem set in homogeneous media and developed by Boyer-Fabrie.</p>
      </subsection>
      <subsection id="cid14" level="2">
        <bodyTitle>Asymptotic modeling in electromagnetism</bodyTitle>
        <participants>
          <person key="poems-2006-idm290075532848">
            <firstname>Marc</firstname>
            <lastname>Duruflé</lastname>
          </person>
          <person key="mc2-2009-idm136144588192">
            <firstname>Victor</firstname>
            <lastname>Péron</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Clair</firstname>
            <lastname>Poignard</lastname>
          </person>
        </participants>
        <p>We investigate asymptotic models for 3D transmission problems in electromagnetism with homogeneous thin layers (uniform thickness). We exhibit Generalized Impedance Boundary Conditions of order 1 when the thin layer is symmetric and non-symmetric with respect to its mean surface. We present also a limit model for a resistive thin layer, and an equivalent model of order 1 for large contrast in conductivities through the thin layer. We write all these models in a general form. Questions regarding the implementation of the conditions have been addressed carefully. Numerical results with the high-order finite element library Montjoie illustrate the accuracy of the asymptotic models. A paper is in preparation.</p>
      </subsection>
      <subsection id="cid15" level="2">
        <bodyTitle>Absorbing Boundary Conditions for Tilted Transverse Isotropic Elastic Media</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547898016">
            <firstname>Hélène</firstname>
            <lastname>Barucq</lastname>
          </person>
          <person key="magique-3d-2011-idm56653182208">
            <firstname>Lionel</firstname>
            <lastname>Boillot</lastname>
          </person>
          <person key="magique-3d-2006-idm245547847584">
            <firstname>Henri</firstname>
            <lastname>Calandra</lastname>
          </person>
          <person key="magique-3d-2006-idm245547889232">
            <firstname>Julien</firstname>
            <lastname>Diaz</lastname>
          </person>
        </participants>
        <p>The simulation of wave propagation in geophysical media is often performed in domains which are huge compared to the wavelenghts of the problem. It is then necessary to reduce the computational domain to a box. When considering acoustic or elastic isotropic media, this can be done by applying an Absorbing Boundary Condition (ABC) or by adding a Perfectly Matched Layer (PML). However, a realistic representation of the Earth subsurface must include anisotropy and, in particular, the so-called Tilted Transverse Isotropy. Perfectly Matched Layers are known to be unstable for this kind of media and, to the best of our knowledge, no ABC have been proposed yet. We have thus proposed a low-order ABC for TTI media.</p>
        <p>This ABC has been constructed for elliptic TTI media, where the slowness curve of the P-Wave is a rotated ellipse. Then, an appropriate change of variable can be applied in order to transform this ellipse into a circle. The main idea consists in imposing the isotropic ABC in the new system of coordinates and to apply the inverse change of variable in order to obtain the elliptic TTI ABC. We have compared numerically the reflections generated by this new ABC in TTI domain to the ones generated by the classical first order ABC in isotropic domains. The results show that the new ABC performs as well as the classical first order one. Moreover, this ABC seems to be also well-suited to non elliptic TTI media.
These results have been presented at the Congrès Français d'Acoustique <ref xlink:href="#magique-3d-2012-bid37" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, at two workshops <ref xlink:href="#magique-3d-2012-bid38" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>, <ref xlink:href="#magique-3d-2012-bid39" location="biblio" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest"/>.</p>
      </subsection>
      <subsection id="cid16" level="2">
        <bodyTitle>Efficient solution methodology based on a local wave tracking strategy for high-frequency Helmholtz problems.</bodyTitle>
        <participants>
          <person key="magique-3d-2006-idm245547891872">
            <firstname>Mohamed</firstname>
            <lastname>Amara</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Sharang</firstname>
            <lastname>Chaudhry</lastname>
          </person>
          <person key="magique-3d-2006-idm245547889232">
            <firstname>Julien</firstname>
            <lastname>Diaz</lastname>
          </person>
          <person key="magique-3d-2006-idm245547842096">
            <firstname>Rabia</firstname>
            <lastname>Djellouli</lastname>
          </person>
          <person key="PASUSERID">
            <firstname>Steven</firstname>
            <lastname>Fiedler</lastname>
          </person>
        </participants>
        <p>We have designed a new and efficient solution
methodology for solving high-frequency Helmholtz
problems. The proposed method is a least-squares
based technique that employs variable bases of
plane waves at the element level of the domain
partition. A local wave tracking strategy is
adopted for the selection of the basis at the
regional/element level. More specifically, for
each element of the mesh partition, a basis of
plane waves is chosen so that one of the plane
waves in the basis is oriented in the direction of
the propagation of the field inside the considered
element. The determination of the direction of the
field inside the mesh partition is formulated as a
minimization problem. Since the problem is
nonlinear, we apply Newton's method to determine
the minimum. The computation of Jacobians and
Hessians that arise in the iterations of the
Newton's method is based on the exact
characterization of the Fréchet derivatives of
the field with respect to the propagation
directions. Such a characterization is crucial for
the stability, fast convergence, and computational
efficiency of the Newton algorithm. These results are part of the Master thesis of Sharang Chaudhry (student à CSUN) and have been presented to the 6th European Congress on
Computational Methods in
Applied Sciences and Engineering (ECCOMAS, Vienna, 2012).</p>
      </subsection>
    </subsection>
    <subsection id="uid32" level="1">
      <bodyTitle>High
Performance methods for solving wave equations</bodyTitle>
      <participants>
        <person key="magique-3d-2011-idm56653182208">
          <firstname>Lionel</firstname>
          <lastname>Boillot</lastname>
        </person>
        <person key="magique-3d-2006-idm245547898016">
          <firstname>Hélène</firstname>
          <lastname>Barucq</lastname>
        </person>
        <person key="magique-3d-2006-idm245547847584">
          <firstname>Henri</firstname>
          <lastname>Calandra</lastname>
        </person>
        <person key="magique-3d-2006-idm245547889232">
          <firstname>Julien</firstname>
          <lastname>Diaz</lastname>
        </person>
        <person key="magique-3d-2010-idm149280180368">
          <firstname>Emiljana</firstname>
          <lastname>Jorgji</lastname>
        </person>
        <person key="gallium-2006-idm16698279520">
          <firstname>Didier</firstname>
          <lastname>Rémy</lastname>
        </person>
        <person key="magique-3d-2010-idm149280189552">
          <firstname>Florent</firstname>
          <lastname>Ventimiglia</lastname>
        </person>
      </participants>
      <p>We have recently optimized the DG code implemented in the DIVA plateform of Total by reducing the number of communications between each processors. Since this code is based on the first order formulation of the elastodynamic wave equation, we have to compute three velocities and six stresses at each degree of freedom of the mesh. One naive idea consists in communicating these nine values at each time step. On the other hand, the computation of the three velocities does not actually require the knowledge of the six stresses but of three linear combination of these stresses. Similarly, the computation of the stresses requires the knowledge of six linear combinations of the three velocities. The main idea of the optimization consists in computing the three linear combinations of the stresses and to communicate them to the other processors, while the three velocities are communicated before computing the linear computations. Hence the number of communications can be reduced to six at each time step.</p>
      <p>This optimization, coupled with the use of Hybrid MPI and OpenMP parallel programming has allowed to prove the scalability of the code up to 512 cores. We are now planning to extend these tests up to 4000 cores.</p>
    </subsection>
  </resultats>
  <contrats id="uid33">
    <bodyTitle>Bilateral Contracts and Grants with Industry</bodyTitle>
    <subsection id="uid34" level="1">
      <bodyTitle>Contracts with TOTAL</bodyTitle>
      <simplelist>
        <li id="uid35">
          <p noindent="true">Depth Imaging Partnership (DIP)</p>
          <p>Period: 2010 January - 2012 december, Management:
Inria Bordeaux Sud-Ouest, Amount: 3600000 euros.
150 000 euros have been devoted to hire an
associate engineer (from Oct. 2010 to Sept. 2012).</p>
        </li>
        <li id="uid36">
          <p noindent="true">Schémas en temps d'ordre élevé pour la
simulation d'ondes élastiques en milieux
fortement hétérogènes par des méthodes DG.</p>
          <p>Period: 2010 November - 2013 October, Management: Inria Bordeaux Sud-Ouest, Amount: 150000 euros.</p>
        </li>
        <li id="uid37">
          <p noindent="true">Propagateurs optimisés pour les ondes élastiques en milieux anisotropes</p>
          <p>Period: 20November - 2014 October, Management: Inria Bordeaux Sud-Ouest, Amount: 160000 euros.</p>
        </li>
        <li id="uid38">
          <p noindent="true">RTM en milieux hétérogènes par équations d'ondes élastiques</p>
          <p>Period: 2011 November - 2014 October, Management: Inria Bordeaux Sud-Ouest, Amount: 160000 euros.</p>
        </li>
      </simplelist>
    </subsection>
  </contrats>
  <partenariat id="uid39">
    <bodyTitle>Partnerships and Cooperations</bodyTitle>
    <subsection id="uid40" level="1">
      <bodyTitle>Regional Initiatives</bodyTitle>
      <p>The PhD fellowship of Elodie Estecahandy is
partially (50%) financed by the Conseil Régional d'Aquitaine.</p>
      <p>The PhD fellowship of Vanessa Mattesi is
partially (50%) financed by the Conseil Régional d'Aquitaine.</p>
      <p>The Post-Doctoral fellowship of Juliette Chabassier is partially (50%) financed by the Conseil Général des Pyrénées Atlantiques.</p>
      <p>The Post-Doctoral fellowship of Ángel Rodríguez Rozas is partially (50%) financed by the Conseil Régional d'Aquitaine.
</p>
    </subsection>
    <subsection id="uid41" level="1">
      <bodyTitle>National Initiatives</bodyTitle>
      <subsection id="uid42" level="2">
        <bodyTitle>Depth Imaging Partnership</bodyTitle>
        <p>Magique-3D maintains active collaborations with
Total. In the context of depth imaging and with
the collaboration of Henri Calandra from Total,
Magique-3D coordinates research activities
dealing with the development of high-performance
numerical methods for solving wave equations in
complex media. This project involves French
academic researchers in mathematics, computing
and in geophysics, and is funded by Total. Currently, two project-teams are involved: Hiepacs and Nachos.</p>
        <p>In the framework of DIP, three PhD students are working in Magique 3D and two new PhD students have been hired this year. One of them is shared with the project team Nachos (<ref xlink:href="http://www-sop.inria.fr/nachos/" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>www-sop.<allowbreak/>inria.<allowbreak/>fr/<allowbreak/>nachos/</ref>). Moreover, one internship has been realized. Always in the framework of DIP, Magique-3D has a collaboration with Prof. Changsoo Shin who is an expert of Geophysics and works at the Department of Energy resources engineering (College of Engineering, Seoul National University). Jewoo Yoo, who is a first year PhD student advised by Prof.Changsoo Shin, has visited Magique-3D during four months, from November 2011 to February 2012.</p>
        <p noindent="true">The contract ends in 2012 and a second period will start in 2013. We aggreed with Total hat the new contract will be signed for five years and that Magique 3D will strenghten its collaboration with Professor J. Tromp at Princeton on the topic of full wave inversion.</p>
      </subsection>
    </subsection>
    <subsection id="uid43" level="1">
      <bodyTitle>European Initiatives</bodyTitle>
      <subsection id="uid44" level="2">
        <bodyTitle>FP7 Projects</bodyTitle>
        <subsection id="uid45" level="3">
          <bodyTitle>HPC-GA</bodyTitle>
          <sanspuceslist>
            <li id="uid46">
              <p noindent="true">Title: High Performance Computing for Geophysics Applications</p>
            </li>
            <li id="uid47">
              <p noindent="true">Type: PEOPLE</p>
            </li>
            <li id="uid48">
              <p noindent="true">Instrument: International Research Staff Exchange Scheme (IRSES)</p>
            </li>
            <li id="uid49">
              <p noindent="true">Duration: January 2012 - December 2014</p>
            </li>
            <li id="uid50">
              <p noindent="true">Coordinator: Inria
(France)</p>
            </li>
            <li id="uid51">
              <p noindent="true">Others partners: BCAM (Basque Center of Applied Mathematics), Spain; BRGM (Bureau de Recherches Géologiques et Minières), France; ISTerre (Institut des Sciences de la Terre, France;
UFRGS (Federal University of Rio Grande do Sul), Institute of Informatics, Brazil;
UNAM (National Autonomous University of Mexico) , Institute of Geophysics, Mexico;</p>
            </li>
            <li id="uid52">
              <p noindent="true">See also: <ref xlink:href="https://project.inria.fr/HPC-GA/en" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">https://<allowbreak/>project.<allowbreak/>inria.<allowbreak/>fr/<allowbreak/>HPC-GA/<allowbreak/>en</ref></p>
            </li>
            <li id="uid53">
              <p noindent="true">Abstract: Simulating large-scale geophysics phenomenon represents, more than ever, a major concern for our society. Recent seismic activity worldwide has shown how crucial it is to enhance our understanding of the impact of earthquakes. Numerical modeling of seismic 3D waves obviously requires highly specific research efforts in geophysics and applied mathematics, leveraging a mix of various schemes such as spectral elements, high-order finite differences or finite elements.</p>
              <p>But designing and porting geophysics applications on top of nowadays supercomputers also requires a strong expertise in parallel programming and the use of appropriate runtime systems able to efficiently deal with heterogeneous architectures featuring many-core nodes typically equipped with GPU accelerators. The HPC-GA project aims at evaluating the functionalities provided by current runtime systems in order to point out their limitations. It also aims at designing new methods and mechanisms for an efficient scheduling of processes/threads and a clever data distribution on such platforms.</p>
              <p>The HPC-GA project is unique in gathering an international, pluridisciplinary consortium of leading European and South American researchers featuring complementary expertise to face the challenge of designing high performance geophysics simulations for parallel architectures: UFRGS, Inria, BCAM and UNAM. Results of this project will be validated using data collected from real sensor networks. Results will be widely disseminated through high-quality publications, workshops and summer-schools.</p>
            </li>
          </sanspuceslist>
        </subsection>
      </subsection>
      <subsection id="uid54" level="2">
        <bodyTitle>Collaborations in European Programs, except FP7</bodyTitle>
        <p>Joint project with BCAM (Basque Center of Applied
Mathematics) funded by the Conseil Régional
d'Aquitaine and the Basque Government in the
framework of the Aquitaine-Euskadi Call. Total
Amount: 14 000 euros.</p>
        <sanspuceslist>
          <li id="uid55">
            <p noindent="true">Program: Fonds commun de coopération Aquitaine/Euskadi</p>
          </li>
          <li id="uid56">
            <p noindent="true">Project acronym: AKELARRE</p>
          </li>
          <li id="uid57">
            <p noindent="true">Project title: Méthodes numériques innovantes et logiciels performants pour la simulation de la propagation des ondes électromagnétiques en milieux complexes</p>
          </li>
          <li id="uid58">
            <p noindent="true">Duration: février 2011 - février 2013</p>
          </li>
          <li id="uid59">
            <p noindent="true">Coordinator: Hélène Barucq</p>
          </li>
          <li id="uid60">
            <p noindent="true">Other partners: BCAM (Basque Center of Applied
Mathematics), Spain</p>
          </li>
          <li id="uid61">
            <p noindent="true">Abstract:
This project brings together the complementary skills in the field of wave propagation of two research teams which are respectively located in Pau and Bilbao. The main objective of this collaboration is to develop innovative numerical methods and to implement powerful software for the simulation of electromagnetic waves in complex media. These waves play an important role in many industrial applications and the development of such software is of great interest for many industrial enterprises located in the region. Theoretical and practical issues are considered. In particular, we focus on the mathematical analysis of boundary conditions that play a crucial role for accurate numerical simulations of waves.</p>
          </li>
        </sanspuceslist>
        <p>Joint project with the Matheon Research Center in Berlin funded by the European Union in the
framework of the Procope 2012 Call. Total Amount: 4200 euros.</p>
        <sanspuceslist>
          <li id="uid62">
            <p noindent="true">Program: PHC Procope 2012</p>
          </li>
          <li id="uid63">
            <p noindent="true">Project acronym: Procope Inria - TU Berlin</p>
          </li>
          <li id="uid64">
            <p noindent="true">Project title: Procope Inria - TU Berlin</p>
          </li>
          <li id="uid65">
            <p noindent="true">Duration: January 2012 - December 2014</p>
          </li>
          <li id="uid66">
            <p noindent="true">Coordinator: Sébastien Tordeux</p>
          </li>
          <li id="uid67">
            <p noindent="true">Other partners: Matheon Research Center, TU Berlin, Germany</p>
          </li>
          <li id="uid68">
            <p noindent="true">Abstract: This project aims in funding trips between Pau and Berlin. The young research group of Kersten Schmidt and Magique 3D are both specialist of the modeling and the simulation of the wave propagation phenomena. During this program we focus on the modeling of multiperforate plates which are present in the combustion chambers; on the derivation of absorbing boundary conditions for stratified media and on the development of precise numerical methods in the context of the Hardy problem.</p>
          </li>
        </sanspuceslist>
      </subsection>
    </subsection>
    <subsection id="uid69" level="1">
      <bodyTitle>International Initiatives</bodyTitle>
      <subsection id="uid70" level="2">
        <bodyTitle>Inria International Partners</bodyTitle>
        <subsection id="uid71" level="3">
          <bodyTitle>
            <ref xlink:href="http://uppa-inria.univ-pau.fr/m3d/Equipe-associee/index.html" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">MAGIC</ref>
          </bodyTitle>
          <sanspuceslist>
            <li id="uid72">
              <p noindent="true">Title: Advance Modeling in Geophysics</p>
            </li>
            <li id="uid73">
              <p noindent="true">Inria principal investigator: Hélène Barucq</p>
            </li>
            <li id="uid74">
              <p noindent="true">International Partner:</p>
              <sanspuceslist>
                <li id="uid75">
                  <p noindent="true">Institution: California State University at Northridge (United States)</p>
                </li>
                <li id="uid76">
                  <p noindent="true">Laboratory: Department of Mathematics</p>
                </li>
              </sanspuceslist>
            </li>
            <li id="uid77">
              <p noindent="true">Duration: 2006 - 2012</p>
            </li>
            <li id="uid78">
              <p noindent="true">See also: <ref xlink:href="http://uppa-inria.univ-pau.fr/m3d/Equipe-associee/index.html" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>uppa-inria.<allowbreak/>univ-pau.<allowbreak/>fr/<allowbreak/>m3d/<allowbreak/>Equipe-associee/<allowbreak/>index.<allowbreak/>html</ref></p>
            </li>
            <li id="uid79">
              <p noindent="true">The main objective of this collaboration is the design of an efficient solution methodology for solving Helmholtz problems in heterogeneous domains, a key step for solving the inversion in complex tectonics. The proposed research program is based upon the following four pillars:</p>
              <p>1. The design, implementation, and the performance assessment of a new hybrid mixed type method (HMM) for solving Helmholtz problems.
2. The construction of local nonreflecting boundary conditions to equip HMM when solving exterior high-frequency Helmholtz problems.
3. The design of an efficient numerical procedure for full-aperture reconstruction of the acoustic far-field pattern (FFP) when measured in a limited aperture.
4. The characterization of the Fréchet derivative of the elasto-acoustic scattered field with respect to the shape of a given elastic scatterer.</p>
            </li>
          </sanspuceslist>
        </subsection>
      </subsection>
      <subsection id="uid80" level="2">
        <bodyTitle>Participation In International Programs</bodyTitle>
        <subsection id="uid81" level="3">
          <bodyTitle>
            <ref xlink:href="http://uppa-inria.univ-pau.fr/m3d/ConfFR/participants.html" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">GEO3D</ref>
          </bodyTitle>
          <p>Joint project with the Novosibirsk state University in Russia funded by the Poncelet laboratory in the
framework of the Inria Russia Call. Total
Amount: 8000 euros for 2012.</p>
          <sanspuceslist>
            <li id="uid82">
              <p noindent="true">Program: Inria-Russia</p>
            </li>
            <li id="uid83">
              <p noindent="true">Title: Models and numerical simulations in Geosciences: wave propagation in complex media</p>
            </li>
            <li id="uid84">
              <p noindent="true">Inria principal investigator: Sébastien Tordeux</p>
            </li>
            <li id="uid85">
              <p noindent="true">International Partner (Institution - Laboratory - Researcher):</p>
              <sanspuceslist>
                <li id="uid86">
                  <p noindent="true">Novosibirsk State University (Russia (Russian Federation))
- Institute of Numerical Mathematics and Mathematical Geophysics - Yuri Laevsky</p>
                </li>
              </sanspuceslist>
            </li>
            <li id="uid87">
              <p noindent="true">Duration: January 2012 to December 2014</p>
            </li>
            <li id="uid88">
              <p noindent="true">See also: <ref xlink:href="http://uppa-inria.univ-pau.fr/m3d/ConfFR/participants.html" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>uppa-inria.<allowbreak/>univ-pau.<allowbreak/>fr/<allowbreak/>m3d/<allowbreak/>ConfFR/<allowbreak/>participants.<allowbreak/>html</ref></p>
            </li>
            <li id="uid89">
              <p noindent="true">GEO3D is a collaborative project between Magique 3D team-project (Inria Bordeaux Sud-Ouest) and the Institute of Numerical Mathematics and Mathematical Geophysics (Novosibirsk State University) in the context of geosciences. We are mainly interested to the derivation of numerical methods (discontinuous Galerkin approximation, space-time refinement), to the design of direct and inverse high performance solver, and to the modeling of complex media.</p>
            </li>
          </sanspuceslist>
        </subsection>
      </subsection>
    </subsection>
    <subsection id="uid90" level="1">
      <bodyTitle>International Research Visitors</bodyTitle>
      <subsection id="uid91" level="2">
        <bodyTitle>Visits of International Scientists</bodyTitle>
        <simplelist>
          <li id="uid92">
            <p noindent="true">Jewoo Yoo, Ph.D Student at Seoul University spent five months <span class="smallcap" align="left">Magique-3D</span> from December 2011 to April 2012.</p>
          </li>
          <li id="uid93">
            <p noindent="true">Rabia Djellouli spent one week in <span class="smallcap" align="left">Magique-3D</span> in November 2012.</p>
          </li>
          <li id="uid94">
            <p noindent="true">Patrick Dular (Université de Liège) is visiting <span class="smallcap" align="left">Magique-3D</span> from December 2012 to February 2013.</p>
          </li>
        </simplelist>
      </subsection>
    </subsection>
  </partenariat>
  <diffusion id="uid95">
    <bodyTitle>Dissemination</bodyTitle>
    <subsection id="uid96" level="1">
      <bodyTitle>Scientific Animation</bodyTitle>
      <subsection id="uid97" level="2">
        <bodyTitle>Conferences Organization</bodyTitle>
        <simplelist>
          <li id="uid98">
            <p noindent="true">In collaboration with the Institute of Numerical Mathematics and Mathematical Geophysics (Novosibirsk State University), Magique 3D organized the First Russian-French Conference on Mathematical Geophysics, Mathematical Modeling in Continuum Mechanics and Inverse Problems (June 18-22) in Biarritz. This conference was the kick-off meeting of the GEO3D project between the two teams. It focused on direct and inverse problems in mathematical geophysics, mathematical modeling in continuum mechanics, and wave propagation.</p>
            <p>Gathering well recognized specialists with a large spectrum of domain of expertise (geophysical modeling, wave propagation, numerical analysis, large scale problems, inverse problems...), it aimed at creating synergy resulting in theoretical and technological advances in these domains. It initiated discussions and defined joint research projects between French and Russian researchers.</p>
            <p>It gathered around forty participants.</p>
            <p>
              <ref xlink:href="http://uppa-inria.univ-pau.fr/m3d/ConfFR/" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>uppa-inria.<allowbreak/>univ-pau.<allowbreak/>fr/<allowbreak/>m3d/<allowbreak/>ConfFR/</ref>
            </p>
          </li>
          <li id="uid99">
            <p noindent="true">Magique 3d coorganized with the BCAM the Aquitanie-Euskadi Workshop on Applied Mathematics (October 29-31) in Biarritz. It was the closing workshop of the AKELARRE project (Aquitaine-Euskadi fundings), it focused on wave problems which were the subject of the joint project and take place in different areas of applied mathematics (control, finite elements, asymptotic analysis, boundary conditions, high performing computing, ...). and it gathered around 30 participants.</p>
            <p>
              <ref xlink:href="http://uppa-inria.univ-pau.fr/m3d/ConfInriaBcam/" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>uppa-inria.<allowbreak/>univ-pau.<allowbreak/>fr/<allowbreak/>m3d/<allowbreak/>ConfInriaBcam/</ref>
            </p>
          </li>
        </simplelist>
      </subsection>
      <subsection id="uid100" level="2">
        <bodyTitle>Administrative Activities</bodyTitle>
        <simplelist>
          <li id="uid101">
            <p noindent="true">Hélène Barucq is vice-chair of the Inria
evaluation committee.
From 2009 to 2012, she has been member of the panel of experts for the ANR programs "SIMI1 programmes blanc et jeunes chercheurs", <ref xlink:href="http://www.agence-nationale-recherche.fr/programmes-de-recherche/recherches-exploratoires-et-emergentes/" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>www.<allowbreak/>agence-nationale-recherche.<allowbreak/>fr/<allowbreak/>programmes-de-recherche/<allowbreak/>recherches-exploratoires-et-emergentes/</ref>. She is the scientific leader of the strategic action Inria-TOTAL "DIP: Depth Imaging Partnership", <ref xlink:href="http://dip.inria.fr/" location="extern" xlink:type="simple" xlink:show="replace" xlink:actuate="onRequest">http://<allowbreak/>dip.<allowbreak/>inria.<allowbreak/>fr/</ref></p>
          </li>
          <li id="uid102">
            <p noindent="true">Julien Diaz is elected member of the Inria
evaluation committee and member of the CDT (Commission de Développement Technologique of Inria Bordeaux Sud-Ouest.</p>
          </li>
          <li id="uid103">
            <p noindent="true">Victor Peron is member of the CJC (Commission Jeunes Chercheurs) of Inria Bordeaux Sud-Ouest</p>
          </li>
          <li id="uid104">
            <p noindent="true">Sébastien Tordeux is elected member of the
26th section of the CNU.</p>
          </li>
        </simplelist>
      </subsection>
    </subsection>
    <subsection id="uid105" level="1">
      <bodyTitle>Teaching - Supervision - Juries</bodyTitle>
      <subsection id="uid106" level="2">
        <bodyTitle>Teaching</bodyTitle>
        <sanspuceslist>
          <li id="uid107">
            <p noindent="true">Master : Julien Diaz et Sébastien Tordeux, Introduction aux phénomènes de propagation d'ondes, 55 Eq TD, M2,</p>
          </li>
          <li id="uid108">
            <p noindent="true">Master : Victor Peron et Sébastien Tordeux, Analyse numérique fondamentale, 110 Eq. TD, M1, UPPA, France,</p>
          </li>
          <li id="uid109">
            <p noindent="true">Summer School : Sébastien Tordeux, Introduction à l'analyse mathématique de l'équation de Helmholtz, 12 Eq. TD, Ecole d'été de Jaca 2012, Espagne</p>
          </li>
        </sanspuceslist>
      </subsection>
      <subsection id="uid110" level="2">
        <bodyTitle>Supervision</bodyTitle>
        <sanspuceslist>
          <li id="uid111">
            <p noindent="true">HdR : Sébastien Tordeux, Modélisation asymptotique pôur les problèmes de propagation d'ondes, Université de Pau et des Pays de l'Adour, January 2012.</p>
          </li>
          <li id="uid112">
            <p noindent="true">PhD in progress : Julien Alvarez, <formula type="inline"><math xmlns="http://www.w3.org/1998/Math/MathML" overflow="scroll"><mrow><mi>h</mi><mi>p</mi></mrow></math></formula>-adaptive inversion of magnetotelluric measurements, October 2011, Hélène Barucq and David Pardo.</p>
          </li>
          <li id="uid113">
            <p noindent="true">PhD in progress : Lionel Boillot, Propagateurs optimisés pour les ondes élastiques en milieux anisotropes, May 2011, Hélène Barucq and Julien Diaz.</p>
          </li>
          <li id="uid114">
            <p noindent="true">PhD in progress : Marie Bonnasse-Gahot, Simulation de la propagation d’ondes élastiques et visco-élastiques
en régime harmonique par des méthodes Galerkin discontinues d’ordre élevé en maillage non-structuré adaptées au calcul haute performance, October 2012, Julien Diaz and Stéphane Lantéri.</p>
          </li>
          <li id="uid115">
            <p noindent="true">PhD in progress : Théophile Chaumont Frélet, , October 2012, Hélène Barucq and Christian Gout.</p>
          </li>
          <li id="uid116">
            <p noindent="true">PhD in progress : Élodie Estecahandy, Sur la rśolution de problèmes de diffraction inverses avec des
angles d'ouverture réduits, October 2010, Hélène Barucq and Rabia Djellouli.</p>
          </li>
          <li id="uid117">
            <p noindent="true">PhD in progress : Jérôme Luquel, RTM en milieu hétérogène par équations d'ondes élastiques, November 2011, Hélène Barucq and Julien Diaz.</p>
          </li>
          <li id="uid118">
            <p noindent="true">PhD in progress : Vanessa Mattesi, détection des hétérogéenéeités en
acoustique et élastodynamique, October 2011, Hélène Barucq and Sébastien Tordeux.</p>
          </li>
          <li id="uid119">
            <p noindent="true">PhD in progress : Florent Ventimiglia, Schémas d'ordre élevé et pas de temps local pour les ondes élastiques en milieux hétérogènes, November 2010, Hélène Barucq and Julien Diaz.</p>
          </li>
        </sanspuceslist>
      </subsection>
      <subsection id="uid120" level="2">
        <bodyTitle>Juries</bodyTitle>
        <simplelist>
          <li id="uid121">
            <p noindent="true">Hélène Barucq was jury member for the PhD defense of</p>
            <simplelist>
              <li id="uid122">
                <p noindent="true">Sébastien Impériale, Modélisation mathématique et numérique de capteurs piézoélectriques, January 2012 (Université de Paris Dauphine).</p>
              </li>
              <li id="uid123">
                <p noindent="true">Sébastien Cambon, Méthodes
d'élements finis d'ordre élevé et d'équations
intégrales pour la résolution de problèmes de
furtivité radar d'objets à symétrie de
révolution, July 2nd 2012 (Université de
Toulouse).</p>
              </li>
              <li id="uid124">
                <p noindent="true">Mohamed Hansbo, Sur le modèle de
Kerr-Debye pour la propagation des ondes
électromagnétiques, October 1st 2012 (Université de Bordeaux).</p>
              </li>
              <li id="uid125">
                <p noindent="true">Dimitri Nicolas, Couplage de méthodes
d'échantillonnage et de méthodes d'optimisation
de formes pour des problèmes de diffraction
inverses, November 28th 2012 (École polytechnique).</p>
              </li>
            </simplelist>
          </li>
          <li id="uid126">
            <p noindent="true">Sébastien Tordeux
was jury member for the PhD defense of</p>
            <simplelist>
              <li id="uid127">
                <p noindent="true">Pierre-Henri Cocquet, Étude mathématique et numérique homogénéisé de métamatériaux, December 7th 2012 (Université de Toulouse).</p>
              </li>
            </simplelist>
          </li>
        </simplelist>
      </subsection>
    </subsection>
    <subsection id="uid128" level="1">
      <bodyTitle>Popularization</bodyTitle>
      <simplelist>
        <li id="uid129">
          <p noindent="true">Hélène Barucq, Lycée Cassin à Bayonne,
conférence pour des classes de seconde,
première et terminale, sur l'application des
mathématiques dans la vie courante, April 6th 2012;</p>
        </li>
        <li id="uid130">
          <p noindent="true">Hélène Barucq, Médiathèque de
Cambo-les-Bains, Cycle Café des Sciences, "Les
mathématiques, ça sert!!!", April 6th 2012.</p>
        </li>
      </simplelist>
    </subsection>
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