{"id":91,"date":"2015-07-22T15:53:46","date_gmt":"2015-07-22T15:53:46","guid":{"rendered":"http:\/\/airborne.geophysicsgpr.com\/?page_id=91"},"modified":"2017-03-09T15:31:58","modified_gmt":"2017-03-09T15:31:58","slug":"helimager","status":"publish","type":"page","link":"https:\/\/airborne.geophysicsgpr.com\/fr\/techniques\/magnetometrie\/helimager\/","title":{"rendered":"Lev\u00e9 a\u00e9romagn\u00e9tique (H\u00e9liMAGer)"},"content":{"rendered":"<div id=\"pl-91\"  class=\"panel-layout\" ><div id=\"pg-91-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-91-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-91-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div class=\"texte-home-right article panel-widget-style panel-widget-style-for-91-0-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p>Le syst\u00e8me H\u00e9liMAGer \u2122 se compose d'une plate-forme de vecteurs h\u00e9liport\u00e9e stable, d\u00e9velopp\u00e9e par G\u00e9ophysique GPR International Inc, con\u00e7ue pour accueillir une gamme de capteurs et instruments diff\u00e9rents, particuli\u00e8rement utiles pour la cartographie et l'exploration des r\u00e9gions montagneuses (Mouge et Chalifoux, 2005). La plate-forme permet la disposition des capteurs dans trois directions orthogonales. Ce syst\u00e8me est g\u00e9n\u00e9ralement configur\u00e9 comme un gradiom\u00e8tre magn\u00e9tique horizontal.<\/p>\n<p>Les avantages de la mesure des gradients horizontaux permettent la production de la carte du champ magn\u00e9tique rehauss\u00e9 qui fournit plus d'informations spatiales que le champ magn\u00e9tique total conventionnel. L\u2019am\u00e9lioration des donn\u00e9es du champ magn\u00e9tique est utile pour identifier plus pr\u00e9cis\u00e9ment l'emplacement de petites anomalies, des contacts, des dykes et des failles entre les lignes de vol.<\/p>\n<p>Pour ce faire, deux (2) capteurs Geometrics G-823A (pompage optique \u00e0 vapeur de c\u00e9sium) de champ magn\u00e9tique total avec un intervalle d'\u00e9chantillonnage de 0,1 seconde est mont\u00e9s \u00e0 6 m\u00e8tres d'intervalle sur le gradiom\u00e8tre, en-dessous d'un c\u00e2ble de 30 m\u00e8tres sous l'h\u00e9licopt\u00e8re. Les magn\u00e9tom\u00e8tres comprennent le capteur G-823A de haute performance de petite taille CM-201 muni d\u2019un compteur Larmor. Le magn\u00e9tom\u00e8tre envoie l'intensit\u00e9 du champ magn\u00e9tique mesur\u00e9 en unit\u00e9s nanotesla (nT), directement au syst\u00e8me d'acquisition de donn\u00e9es via un port RS-232. Il offre une polyvalence in\u00e9gal\u00e9e de performance, de taille et de fonction.<\/p>\n<h2 class=\"h2resize\">H\u00e9liMAGer est un donc un syst\u00e8me de choix pour tout lev\u00e9 magn\u00e9tique h\u00e9liport\u00e9 \u00e0 garde au sol serr\u00e9 de haute r\u00e9solution.<\/h2>\n<p>La prise de mesures de gradient permet de s\u2019affranchir en bonne partie de l\u2019erreur sur la composante temporelle appel\u00e9e effet diurne, puisque les gradients ne sont pas affect\u00e9s par celui-ci. Les lev\u00e9s gradiom\u00e9triques s\u2019affranchissent donc de l\u2019obligation d\u2019une station de base.<\/p>\n<p>\u00a0<\/p>\n<p>\u00a0<\/p>\n<p>Pour plus d'informations, veuillez contacter notre <a style=\"color: #3a5568\" href=\"mailto:info@geophysicsgpr.com\">\u00c9quipe de lev\u00e9 a\u00e9roport\u00e9<\/a>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-91-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-91-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-91-1-0-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"1\" ><div class=\"panel-widget-style panel-widget-style-for-91-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-91\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/enhanced.jpg\" width=\"1487\" height=\"753\" srcset=\"https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/enhanced.jpg 1487w, https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/enhanced-300x152.jpg 300w, https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/enhanced-1024x519.jpg 1024w\" sizes=\"auto, (max-width: 1487px) 100vw, 1487px\" title=\"Airborne_techniques_helimager\" alt=\"H\u00e9limager\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-91-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-91-1-1-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"2\" ><div class=\"panel-widget-style panel-widget-style-for-91-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-91\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/IMG_0039.jpg\" width=\"2592\" height=\"1944\" srcset=\"https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/IMG_0039.jpg 2592w, https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/IMG_0039-300x225.jpg 300w, https:\/\/airborne.geophysicsgpr.com\/wp-content\/uploads\/sites\/8\/2015\/07\/IMG_0039-1024x768.jpg 1024w\" sizes=\"auto, (max-width: 2592px) 100vw, 2592px\" title=\"Airborne_techniques_helimager\" alt=\"H\u00e9limager\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Le syst\u00e8me H\u00e9liMAGer \u2122 se compose d&rsquo;une plate-forme de vecteurs h\u00e9liport\u00e9e stable, d\u00e9velopp\u00e9e par G\u00e9ophysique GPR International Inc, con\u00e7ue pour accueillir une gamme de capteurs et instruments diff\u00e9rents, particuli\u00e8rement utiles pour la cartographie et l&rsquo;exploration des r\u00e9gions montagneuses (Mouge et Chalifoux, 2005). La plate-forme permet la disposition des capteurs dans trois directions orthogonales. Ce syst\u00e8me&#8230;  <a href=\"https:\/\/airborne.geophysicsgpr.com\/fr\/techniques\/magnetometrie\/helimager\/\" class=\"more-link\" title=\"Read Lev\u00e9 a\u00e9romagn\u00e9tique (H\u00e9liMAGer)\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":632,"parent":77,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-91","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/91","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/comments?post=91"}],"version-history":[{"count":15,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/91\/revisions"}],"predecessor-version":[{"id":1018,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/91\/revisions\/1018"}],"up":[{"embeddable":true,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/77"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media\/632"}],"wp:attachment":[{"href":"https:\/\/airborne.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media?parent=91"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}