{"id":125,"date":"2015-07-22T17:46:51","date_gmt":"2015-07-22T16:46:51","guid":{"rendered":"http:\/\/marine.geophysicsgpr.com\/?page_id=125"},"modified":"2017-03-09T17:23:41","modified_gmt":"2017-03-09T16:23:41","slug":"magnetometrie","status":"publish","type":"page","link":"https:\/\/marine.geophysicsgpr.com\/fr\/techniques-geophysiques-marine\/magnetometrie","title":{"rendered":"Magn\u00e9tom\u00e9trie"},"content":{"rendered":"<div id=\"pl-125\"  class=\"panel-layout\" ><div id=\"pg-125-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-125-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-125-0-0-0\" 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-125-0-0-0\" ><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>Les variations locales du champ magn\u00e9tique de la Terre sont souvent caus\u00e9es par la proximit\u00e9 d\u2019objets ferromagn\u00e9tiques ou magn\u00e9tiques. En mesurant et en enregistrant ces variations, il est alors possible de d\u00e9tecter la pr\u00e9sence d\u2019objets et de s\u00e9diments immerg\u00e9s. En rattachant les valeurs de position du capteur aux variations magn\u00e9tiques, il est possible de concevoir une carte pr\u00e9cise r\u00e9v\u00e9lant la position des objets.<\/p>\n<p>Les lev\u00e9s de magn\u00e9tom\u00e9trie marine sont produits avec un magn\u00e9tom\u00e8tre sp\u00e9cialement adapt\u00e9 aux travaux marins. Le magn\u00e9tom\u00e8tre est install\u00e9 sur un poisson-remorque \u00e9tanche tir\u00e9 par une embarcation reli\u00e9e par un c\u00e2ble. Dans la plupart des cas, il comprend un capteur de type pr\u00e9cession protonique ou Overhauser.<\/p>\n<p><span id=\"result_box\" class=\"\" lang=\"fr\"><span class=\"hps\">Les magn\u00e9tom\u00e8tres<\/span> <span class=\"hps\">ont une gamme<\/span> <span class=\"hps\">tr\u00e8s vari\u00e9e<\/span> <span class=\"hps\">d'applications<\/span>, <span class=\"hps\">y compris<\/span>\u00a0la\u00a0<span class=\"hps\">localisation d'objets<\/span> <span class=\"hps\">tels que<\/span>\u00a0l<span class=\"hps\">es sous-marins<\/span><span class=\"\">,<\/span>\u00a0l<span class=\"hps\">es navires coul\u00e9s<\/span>, les risques <span class=\"hps\">pour les<\/span> <span class=\"hps\">tunneliers<\/span>, les dangers <span class=\"hps\">dans les mines<\/span> <span class=\"hps\">de charbon, les<\/span> <span class=\"hps\">munitions non explos\u00e9es<\/span>, l<span class=\"hps\">es f\u00fbts de d\u00e9chets<\/span> <span class=\"hps\">toxiques<\/span>, <span class=\"hps\">ainsi qu'un<\/span> <span class=\"hps\">large \u00e9ventail de<\/span> <span class=\"hps\">gisements min\u00e9raux<\/span> <span class=\"hps\">et de structures<\/span> <span class=\"hps\">g\u00e9ologiques<\/span>. <\/span><\/p>\n<p><span class=\"hps\">Ils ont<\/span> <span class=\"hps\">aussi des applications dans<\/span> <span class=\"hps\">moniteurs de rythme<\/span> <span class=\"hps\">cardiaque<\/span>, le positionnement <span class=\"hps\">des<\/span> <span class=\"hps\">syst\u00e8mes d'armes<\/span>, les capteurs <span class=\"hps\">dans<\/span> <span class=\"hps\">les freins<\/span> <span class=\"hps\">antiblocage<\/span>, les\u00a0<span class=\"hps\">pr\u00e9visions<\/span> <span class=\"hps\">m\u00e9t\u00e9o<\/span> <span class=\"hps\">(via<\/span>\u00a0les\u00a0<span class=\"hps\">cycles solaires<\/span>), les\u00a0<span class=\"hps\">pyl\u00f4nes<\/span> <span class=\"hps\">en acier<\/span>, les\u00a0<span class=\"hps\">syst\u00e8mes de guidage<\/span>\u00a0et\u00a0<span class=\"hps\">de forage<\/span>, <span class=\"hps\">l'arch\u00e9ologie<\/span>, <span class=\"hps\">la tectonique des plaques,<\/span>\u00a0<span class=\"hps\">la propagation des ondes<\/span> <span class=\"hps\">radio<\/span> <span class=\"hps\">et l'exploration<\/span> <span class=\"hps\">plan\u00e9taire.<\/span><\/p>\n<p>\u00a0<\/p>\n<h2 class=\"h2resize\">Applications de la magn\u00e9tom\u00e9trie :<\/h2>\n<ul>\n<li>Arch\u00e9ologie;<\/li>\n<li>\u00c9tude en g\u00e9nie;<\/li>\n<li>\u00c9tude g\u00e9ologique;<\/li>\n<li>Exploration mini\u00e8re;<\/li>\n<li>Recherche et sauvetage sous-marin.<\/li>\n<\/ul>\n<p>\u00a0<\/p>\n<p>\u00a0<\/p>\n<p>Pour plus d'informations, veuillez contacter notre <span style=\"color: #013ca6\"><a style=\"color: #013ca6\" href=\"mailto:info@geophysicsgpr.com\">\u00c9quipe de lev\u00e9 marin<\/a><\/span>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pgc-125-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-125-0-1-0\" class=\"so-panel widget widget_sow-image panel-first-child\" data-index=\"1\" ><div class=\"panel-widget-style panel-widget-style-for-125-0-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-125\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_techniques_Mag.jpg\" width=\"569\" height=\"640\" srcset=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_techniques_Mag.jpg 569w, https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_techniques_Mag-267x300.jpg 267w\" sizes=\"auto, (max-width: 569px) 100vw, 569px\" title=\"Marine_techniques_Magnetometry\" alt=\"Magn\u00e9tom\u00e9trie\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><div id=\"panel-125-0-1-1\" class=\"so-panel widget widget_sow-image panel-last-child\" data-index=\"2\" ><div class=\"panel-widget-style panel-widget-style-for-125-0-1-1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-125\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_techniques_Mag_inset.jpg\" width=\"225\" height=\"300\" sizes=\"auto, (max-width: 225px) 100vw, 225px\" title=\"Marine_techniques_Magnetometry\" alt=\"Magn\u00e9tom\u00e9trie\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-125-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-125-1-0\"  class=\"panel-grid-cell panel-grid-cell-empty panel-grid-cell-mobile-last\" ><\/div><div id=\"pgc-125-1-1\"  class=\"panel-grid-cell panel-grid-cell-empty\" ><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Les variations locales du champ magn\u00e9tique de la Terre sont souvent caus\u00e9es par la proximit\u00e9 d\u2019objets ferromagn\u00e9tiques ou magn\u00e9tiques. En mesurant et en enregistrant ces variations, il est alors possible de d\u00e9tecter la pr\u00e9sence d\u2019objets et de s\u00e9diments immerg\u00e9s. En rattachant les valeurs de position du capteur aux variations magn\u00e9tiques, il est possible de concevoir&#8230;  <a href=\"https:\/\/marine.geophysicsgpr.com\/fr\/techniques-geophysiques-marine\/magnetometrie\" class=\"more-link\" title=\"Read Magn\u00e9tom\u00e9trie\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":78,"parent":16,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-125","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/125","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/comments?post=125"}],"version-history":[{"count":13,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/125\/revisions"}],"predecessor-version":[{"id":1619,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/125\/revisions\/1619"}],"up":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/16"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media\/78"}],"wp:attachment":[{"href":"https:\/\/marine.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media?parent=125"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}