{"id":2214,"date":"2021-04-27T16:29:04","date_gmt":"2021-04-27T14:29:04","guid":{"rendered":"http:\/\/www.hydrosciences.org\/?p=2214"},"modified":"2021-04-27T16:29:04","modified_gmt":"2021-04-27T14:29:04","slug":"laboratoire-lama-isotropes-stables-chnos","status":"publish","type":"post","link":"https:\/\/www.hydrosciences.org\/?p=2214&lang=fr","title":{"rendered":"Isotopes stables C.H.N.O.S"},"content":{"rendered":"\n<p><strong>Responsable technique : Nicolas PATRIS (IR, IRD)<br>R\u00e9f\u00e9rent Scientifique : Jean-Denis TAUPIN (CR, IRD)<\/strong><\/p>\n\n\n\n<p class=\"justify\">Cette plateforme est constitu\u00e9e de deux composantes d\u00e9di\u00e9es \u00e0 l\u2019analyse des rapports isotopiques dans diff\u00e9rents compartiments des Hydrosyst\u00e8mes (Eaux, S\u00e9diments, Sols\u2026) et des environnements m\u00e9diterran\u00e9ens actuels et pass\u00e9s. Le LAMA (Laboratoire Montpelli\u00e9rain d\u2019Analyse des isotopes de l\u2019eau) est int\u00e9gr\u00e9 \u00e0 HSM, et d\u00e9di\u00e9 \u00e0 la mesure de la composition en isotopes stables de l\u2019eau dans les diff\u00e9rents r\u00e9servoirs du cycle hydrologique pour les projets de recherche d\u2018HydroSciences Montpellier et de ses partenaires autour de la ressource en eau, ou du tra\u00e7age de l\u2019origine et du transport des masses d\u2019eau. La plateforme AETE-ISO de l\u2019OSU OREME comprend \u00e9galement deux spectrom\u00e8tres IRMS de mesure des rapports isotopiques de C, H, O, N, S dans diff\u00e9rents mat\u00e9riaux et matrices organiques ou min\u00e9rales, incluant les carbonates.<\/p>\n\n\n\n<ul class=\"wp-block-list\"><li>Isotopes stables de la mol\u00e9cule d\u2019eau d<sup>18<\/sup>O et d<sup>2<\/sup>H<\/li><li>Rapports isotopiques d<sup>13<\/sup>C, d<sup>2<\/sup>H, d<sup>15<\/sup>N, d<sup>18<\/sup>O, d<sup>34<\/sup>S dans diff\u00e9rents mat\u00e9riaux min\u00e9raux, organiques ou biologiques<\/li><\/ul>\n\n\n\n<p><strong><em>EQUIPEMENTS<\/em><\/strong> :<\/p>\n\n\n\n<p><strong><em>Instruments destin\u00e9s aux isotopes stables de la mol\u00e9cule d\u2019eau disponible \u00e0 HydroSciences :<\/em><\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\"><li><em>IRMS Isoprime (Elementar) associ\u00e9 \u00e0 un banc d\u2019\u00e9quilibration pour la mesure <\/em><em>d<sup>18<\/sup>O de l\u2019eau en mode Dual Inlet, et \u00e0 un analyseur \u00e9l\u00e9mentaire PyrOH (Eurovector) pour la mesure <\/em><em>d<sup>2<\/sup>H de l\u2019eau en Flux Continu.<\/em><em><\/em><\/li><li><em>Picarro (spectroscopie laser CRDS) en capacit\u00e9 de r\u00e9aliser des mesures sur l\u2019eau liquide et sur l\u2019eau en phase vapeur, \u00e9quip\u00e9 d\u2019un vaporisateur et d\u2019un passeur liquide automatique.<\/em><\/li><\/ul>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-large is-style-default\"><img decoding=\"async\" src=\"http:\/\/www.hydrosciences.org\/wp-content\/uploads\/image-10.png\" alt=\"\" class=\"wp-image-2034\"\/><figcaption><em>Spectrom\u00e8tre de masse Isoprime coupl\u00e9 au PyrOH Eurovector<\/em><br><em>Mesure en flux continu de d<sup>2<\/sup>H de la mol\u00e9cule d\u2019eau<\/em><\/figcaption><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-large is-style-default\"><img decoding=\"async\" src=\"http:\/\/www.hydrosciences.org\/wp-content\/uploads\/image-11-edited-2.png\" alt=\"\" class=\"wp-image-2293\"\/><figcaption><em><em>Picarro L2130i avec passeur liquide<\/em><br><em>Mesures simultan\u00e9es d<sup>18<\/sup>O et d<sup>2<\/sup>H de la mol\u00e9cule d\u2019eau<\/em><\/em><\/figcaption><\/figure>\n<\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p><strong><em>Instruments destin\u00e9s \u00e0 l\u2019analyse des isotopes (C,H,O,N,S) de la mati\u00e8re organique ou min\u00e9rale et des carbonates, disponibles sur la plateforme AETE-ISO de l\u2019OSU OREME :<\/em><\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\"><li><em>Delta V Plus (ThermoScientific) associ\u00e9 \u00e0 2 Analyseurs El\u00e9mentaires (un Flash IRMS&nbsp; pour les analyses <\/em><em>d<sup>13<\/sup>C, <\/em><em>d<sup>15<\/sup>N et <\/em><em>d<sup>34<\/sup>S par combustion, et un TC\/EA<\/em><em> pour les analyses <\/em><em>d<sup>2<\/sup>H et <\/em><em>d<sup>18<\/sup>O<\/em><em> par pyrolyse)<\/em><\/li><li><em>Delta V Plus (ThermoScientific) avec pr\u00e9parateur automatis\u00e9 pour micro-carbonates (20 microgrammes) de type Kiel IV, pour les analyses <\/em><em>d<sup>13<\/sup>C et <\/em><em>d<sup>18<\/sup>O du carbonate.<strong><\/strong><\/em><\/li><\/ul>\n\n\n\n<p><\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-vertically-aligned-top is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-large is-resized\"><img fetchpriority=\"high\" decoding=\"async\" src=\"http:\/\/www.hydrosciences.org\/wp-content\/uploads\/image-12.png\" alt=\"\" class=\"wp-image-2040\" width=\"274\" height=\"271\"\/><figcaption><em>IRMS Delta V coupl\u00e9 au KIEL Thermo Scientific pour l\u2019analyse&nbsp; d<sup>18<\/sup>O et d<sup>13<\/sup>C des carbonates<\/em><\/figcaption><\/figure>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Responsable technique : Nicolas PATRIS (IR, IRD)R\u00e9f\u00e9rent Scientifique : Jean-Denis TAUPIN (CR, IRD) Cette plateforme est constitu\u00e9e de deux composantes d\u00e9di\u00e9es \u00e0 l\u2019analyse des rapports isotopiques dans diff\u00e9rents compartiments des Hydrosyst\u00e8mes (Eaux, S\u00e9diments, Sols\u2026) et des environnements m\u00e9diterran\u00e9ens actuels et pass\u00e9s. Le LAMA (Laboratoire Montpelli\u00e9rain d\u2019Analyse des isotopes de l\u2019eau) est int\u00e9gr\u00e9 \u00e0 HSM, et &hellip;<\/p>\n<p class=\"read-more\"> <a class=\"\" href=\"https:\/\/www.hydrosciences.org\/?p=2214&#038;lang=fr\"> <span class=\"screen-reader-text\">Isotopes stables C.H.N.O.S<\/span> Lire la suite \u00bb<\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"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":[78],"tags":[],"class_list":["post-2214","post","type-post","status-publish","format-standard","hentry","category-plateau-technique-abihs"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v26.2 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Isotopes stables C.H.N.O.S - HydroSciences Montpellier<\/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:\/\/www.hydrosciences.org\/?p=2214&lang=fr\" \/>\n<meta property=\"og:locale\" content=\"fr_FR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Isotopes stables C.H.N.O.S - HydroSciences Montpellier\" \/>\n<meta property=\"og:description\" content=\"Responsable technique : Nicolas PATRIS (IR, IRD)R\u00e9f\u00e9rent Scientifique : Jean-Denis TAUPIN (CR, IRD) Cette plateforme est constitu\u00e9e de deux composantes d\u00e9di\u00e9es \u00e0 l\u2019analyse des rapports isotopiques dans diff\u00e9rents compartiments des Hydrosyst\u00e8mes (Eaux, S\u00e9diments, Sols\u2026) et des environnements m\u00e9diterran\u00e9ens actuels et pass\u00e9s. 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