{"id":240,"date":"2021-01-05T10:58:03","date_gmt":"2021-01-05T09:58:03","guid":{"rendered":"http:\/\/hebergement.universite-paris-saclay.fr\/upgeo\/?page_id=240"},"modified":"2021-01-05T12:26:58","modified_gmt":"2021-01-05T11:26:58","slug":"tache-1-geologie-et-modelisation-reservoir","status":"publish","type":"page","link":"https:\/\/hebergement.universite-paris-saclay.fr\/upgeo\/?page_id=240","title":{"rendered":"T\u00e2che 1. G\u00e9ologie et mod\u00e9lisation r\u00e9servoir"},"content":{"rendered":"\n

Les objectifs seront de caract\u00e9riser l’\u00e9coulement pass\u00e9 des fluides \u00e0 l’origine des ciments carbonat\u00e9s et des p\u00e9riodes de dissolution et de fournir un ou plusieurs mod\u00e8les g\u00e9ologiques statistiques pour deux types de r\u00e9servoirs (1) carbonat\u00e9 et (2) gr\u00e9seux, principalement en France. Les donn\u00e9es diagraphiques des puits disponibles dans ces bassins seront int\u00e9gr\u00e9es dans la base de donn\u00e9es disponible \u00e0 GEOPS (actuellement 800 puits dans Petrel). L’\u00e9tude des faci\u00e8s et des microfaci\u00e8s permettra d’\u00e9tablir des mod\u00e8les g\u00e9ostatistiques avec des param\u00e8tres, notamment de porosit\u00e9 et perm\u00e9abilit\u00e9, qui d\u00e9pendront des environnements de d\u00e9p\u00f4t et de la composition chimique et min\u00e9ralogique. Une fois les lois statistiques \u00e9tablies, les effets de la variabilit\u00e9 spatiale des propri\u00e9t\u00e9s des r\u00e9servoirs pourront \u00eatre \u00e9tudi\u00e9s par une approche Monte-Carlo pour cr\u00e9er des mod\u00e8les utilis\u00e9s pour les calculs hydrodynamiques et thermiques. Cette t\u00e2che devra prendre en compte l’h\u00e9t\u00e9rog\u00e9n\u00e9it\u00e9 des faci\u00e8s s\u00e9dimentaires, leur diagen\u00e8se (faci\u00e8s oolithiques ciment\u00e9s, non ciment\u00e9s, \u00eelots \u00e9merg\u00e9s, lagunes, barres d’estuaire, argiles dans l’espace intergranulaire), les circulations et thermicit\u00e9 pass\u00e9es et leur degr\u00e9 de fracturation.<\/p>\n","protected":false},"excerpt":{"rendered":"

Les objectifs seront de caract\u00e9riser l’\u00e9coulement pass\u00e9 des fluides \u00e0 l’origine des ciments carbonat\u00e9s et des p\u00e9riodes de dissolution et de fournir un ou plusieurs mod\u00e8les g\u00e9ologiques statistiques pour deux types de r\u00e9servoirs (1) carbonat\u00e9 et (2) gr\u00e9seux, principalement en France. Les donn\u00e9es diagraphiques des puits disponibles dans ces bassins seront int\u00e9gr\u00e9es dans la base […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":244,"menu_order":1,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-240","page","type-page","status-publish","hentry","post-preview"],"yoast_head":"\nT\u00e2che 1. G\u00e9ologie et mod\u00e9lisation r\u00e9servoir - UPGEO<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/hebergement.universite-paris-saclay.fr\/upgeo\/?page_id=240\" \/>\n<meta property=\"og:locale\" content=\"fr_FR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"T\u00e2che 1. G\u00e9ologie et mod\u00e9lisation r\u00e9servoir - UPGEO\" \/>\n<meta property=\"og:description\" content=\"Les objectifs seront de caract\u00e9riser l’\u00e9coulement pass\u00e9 des fluides \u00e0 l’origine des ciments carbonat\u00e9s et des p\u00e9riodes de dissolution et de fournir un ou plusieurs mod\u00e8les g\u00e9ologiques statistiques pour deux types de r\u00e9servoirs (1) carbonat\u00e9 et (2) gr\u00e9seux, principalement en France. 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