{"id":3480,"date":"2021-12-01T15:54:15","date_gmt":"2021-12-01T14:54:15","guid":{"rendered":"http:\/\/www.hydrosciences.org\/?p=3480"},"modified":"2024-11-18T14:56:48","modified_gmt":"2024-11-18T13:56:48","slug":"couplage-entre-tomographies-hydrauliques-et-mesures-hydrodynamiques-pour-la-caracterisation-du-champ-de-permeabilite-de-reservoirs-geologiques-heterogenes-mise-en-oeuvre-en-contexte-sedimentaire-coti","status":"publish","type":"post","link":"https:\/\/www.hydrosciences.org\/?p=3480&lang=fr","title":{"rendered":"Couplage entre tomographies hydrauliques et mesures hydrodynamiques pour la caract\u00e9risation du champ de perm\u00e9abilit\u00e9 de r\u00e9servoirs g\u00e9ologiques h\u00e9t\u00e9rog\u00e8nes. Mise en \u0153uvre en contexte s\u00e9dimentaire c\u00f4tier – Mohammed ALIOUACHE"},"content":{"rendered":"\n

Soutenance de th\u00e8se<\/strong>, le 17 D\u00e9cembre 2021<\/strong> \u00e0 partir de 9h00, Salle de Conf\u00e9rence de la Maison des Sciences de l’Eau + visio conf\u00e9rence<\/p>\n\n\n\n

R\u00e9sum\u00e9 <\/strong><\/p>\n\n\n\n

La perm\u00e9abilit\u00e9 des milieux matriciels s\u00e9dimentaires peut \u00eatre estim\u00e9e in situ <\/em>par l\u2019interm\u00e9diaire d\u2019essais hydrauliques permettant d\u2019acc\u00e9der \u00e0 une perm\u00e9abilit\u00e9 \u00e9quivalente du milieu investigu\u00e9. Cette perm\u00e9abilit\u00e9 peut localement pr\u00e9senter des diff\u00e9rences importantes du fait de l\u2019h\u00e9t\u00e9rog\u00e9n\u00e9it\u00e9 du milieu et de l\u2019\u00e9chelle d\u2019investigation associ\u00e9e aux essais.<\/p>\n\n\n\n

Le pr\u00e9sent travail de doctorat propose une m\u00e9thodologie de caract\u00e9risation spatiale du champ de perm\u00e9abilit\u00e9 en contexte s\u00e9dimentaire, bas\u00e9e sur la mise en place de mod\u00e8les num\u00e9riques par tomographies hydrauliques int\u00e9grant des donn\u00e9es g\u00e9ologiques, g\u00e9ophysiques, p\u00e9trophysiques et hydrauliques, acquises \u00e0 diff\u00e9rentes \u00e9chelles spatio-temporelles. Ces mod\u00e8les visent in fine <\/em>\u00e0 imager la distribution spatiale des propri\u00e9t\u00e9s hydrodynamiques, contrainte par la distribution des facies s\u00e9dimentaires \u00e0 l\u2019\u00e9chelle du r\u00e9servoir g\u00e9ologique.<\/p>\n\n\n\n

L\u2019approche propos\u00e9e est tout d\u2019abord mise en \u0153uvre sur des mod\u00e8les synth\u00e9tiques afin d\u2019en appr\u00e9cier les performances et les limites, puis appliqu\u00e9e \u00e0 un site exp\u00e9rimental, situ\u00e9 en contexte de plate-forme carbonat\u00e9e. Les donn\u00e9es de rabattements acquises lors d\u2019essais de pompages, renseignent sur l\u2019organisation horizontale du champ de perm\u00e9abilit\u00e9. Elles sont compl\u00e9t\u00e9es par des mesures de d\u00e9bitm\u00e8tre le long des forages qui permettent de pr\u00e9ciser la distribution verticale des perm\u00e9abilit\u00e9s. Les r\u00e9sultats obtenus sont compar\u00e9s aux mesures des propri\u00e9t\u00e9s p\u00e9trophysiques r\u00e9alis\u00e9es sur les diff\u00e9rents puits carott\u00e9s du site exp\u00e9rimental. La bonne ad\u00e9quation entre les mod\u00e8les et les mesures de terrain valide l\u2019approche propos\u00e9e comme un moyen efficace et \u00e9conomique pour caract\u00e9riser le champ de perm\u00e9abilit\u00e9s en 3D.<\/p>\n\n\n\n

L\u2019application de cette approche \u00e0 des r\u00e9ponses hydrodynamiques en domaine transitoire s\u2019accompagne d\u2019instabilit\u00e9s num\u00e9riques du probl\u00e8me inverse, l\u2019inversion \u00e9tant assujettie \u00e0 des probl\u00e9matiques de non-unicit\u00e9 de solution. Une \u00e9tude investiguant ces instabilit\u00e9s est r\u00e9alis\u00e9e au moyen de diff\u00e9rentes approches qui montrent que les r\u00e9ponses hydrauliques pour les temps longs sont contr\u00f4l\u00e9es par les conditions aux limites du syst\u00e8me mais \u00e9galement par l\u2019h\u00e9t\u00e9rog\u00e9n\u00e9it\u00e9 \u00e0 m\u00e9so-\u00e9chelle, et notamment la g\u00e9om\u00e9trie des dunes carbonat\u00e9es Une m\u00e9thode d\u2019inversion plus stable sur le plan num\u00e9rique et int\u00e9grant l\u2019h\u00e9t\u00e9rog\u00e9n\u00e9it\u00e9 \u00e0 diff\u00e9rentes \u00e9chelles est ainsi propos\u00e9e.<\/p>\n\n\n\n

Jury <\/strong><\/p>\n\n\n\n

\n
\n
\n
\n
Philippe RENARD<\/strong>, Professeur, Universit\u00e9 de Neuch\u00e2tel, Suisse – Rapporteur
Abderrahim JARDANI<\/strong>, Maitre de conf\u00e9rences HDR, Universit\u00e9 de Rouen Normandie, France – Rapporteur
Christian LEDUC<\/strong>, Directeur de recherche, Institut de Recherche pour le D\u00e9veloppement, France – Examinateur
V\u00e9ronique LEONARDI<\/strong>, Maitre de conf\u00e9rences, Universit\u00e9 de Montpellier, France – Examinatrice
Xiaoguang WANG<\/strong>, Professeur, Universit\u00e9 de Technologie de Chengdu, Chine – Examinateur
Herv\u00e9 JOURDE<\/strong>, Professeur, Universit\u00e9 de Montpellier, France – Directeur de th\u00e8se
Jean-Louis LESUEUR<\/strong>, Ing\u00e9nieur, TotalEnergies CSTJF-PAU, France – Invit\u00e9
Gerard MASSONNAT<\/strong>, Ing\u00e9nieur, TotalEnergies CSTJF-PAU, France  – Invit\u00e9<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n

<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"

Soutenance de th\u00e8se, le 17 D\u00e9cembre 2021 \u00e0 partir de 9h00, Salle de Conf\u00e9rence de la Maison des Sciences de l’Eau + visio conf\u00e9rence R\u00e9sum\u00e9  La perm\u00e9abilit\u00e9 des milieux matriciels s\u00e9dimentaires peut \u00eatre estim\u00e9e in situ par l\u2019interm\u00e9diaire d\u2019essais hydrauliques permettant d\u2019acc\u00e9der \u00e0 une perm\u00e9abilit\u00e9 \u00e9quivalente du milieu investigu\u00e9. Cette perm\u00e9abilit\u00e9 peut localement pr\u00e9senter des diff\u00e9rences importantes …<\/p>\n

Couplage entre tomographies hydrauliques et mesures hydrodynamiques pour la caract\u00e9risation du champ de perm\u00e9abilit\u00e9 de r\u00e9servoirs g\u00e9ologiques h\u00e9t\u00e9rog\u00e8nes. Mise en \u0153uvre en contexte s\u00e9dimentaire c\u00f4tier – Mohammed ALIOUACHE<\/span> Lire la suite \u00bb<\/a><\/p>\n","protected":false},"author":1,"featured_media":3369,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"","footnotes":""},"categories":[27,105],"tags":[],"class_list":["post-3480","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-toutes-les-actualites","category-actualite-these-de-doctorat"],"yoast_head":"\nCouplage entre tomographies hydrauliques et mesures hydrodynamiques pour la caract\u00e9risation du champ de perm\u00e9abilit\u00e9 de r\u00e9servoirs g\u00e9ologiques h\u00e9t\u00e9rog\u00e8nes. 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