{"id":874,"date":"2015-07-21T16:18:38","date_gmt":"2015-07-21T16:18:38","guid":{"rendered":"http:\/\/ground.geophysicsgpr.com\/?page_id=874"},"modified":"2017-02-28T21:38:12","modified_gmt":"2017-02-28T21:38:12","slug":"cartographie-des-vides","status":"publish","type":"page","link":"https:\/\/ground.geophysicsgpr.com\/fr\/techniques-de-geophysique-terrestre\/resistivite-electrique-pp-ps\/cartographie-des-vides","title":{"rendered":"Cartographie des vides"},"content":{"rendered":"<div id=\"pl-874\"  class=\"panel-layout\" ><div id=\"pg-874-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-874-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-874-0-0-0\" 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-874-0-0-0\" ><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<h2 class=\"h2resize\">Exemples d'applications classiques de la cartographie des vides<\/h2>\n<p>La cartographie des vides est une m\u00e9thode \u00e9lectrique de la g\u00e9ophysique terrestre appliqu\u00e9e \u00e0 la quantification des volumes de terrains, les intrusions min\u00e9rales et \u00e0 la cartographie des r\u00e9sistivit\u00e9s apparentes.<\/p>\n<p>Les m\u00e9thodes g\u00e9ophysiques permettent d'identifier et de cartographier efficacement les zones d'affaissement de sols, les vides, les cavit\u00e9s et les karsts; qu'ils soient d'origine naturelle ou caus\u00e9s par l'activit\u00e9 humaine.<\/p>\n<p>La m\u00e9thode \u00e9lectrique est bas\u00e9e sur la mesure en surface de l'intensit\u00e9 et de la diff\u00e9rence de potentiel existantes entre les diff\u00e9rentes \u00e9lectrodes du dispositif de mesure. Le rapport de ces deux param\u00e8tres permet de calculer la r\u00e9sistivit\u00e9 des terrains sous-jacents.<\/p>\n<p>Le choix de la m\u00e9thode n\u00e9cessite la connaissance des conditions de terrain, la g\u00e9ologie r\u00e9gionale et les principes g\u00e9ophysiques applicables.<\/p>\n<p>La r\u00e9sistivit\u00e9 \u00e9lectrique constitue une m\u00e9thode efficace pour cartographier des formations karstiques, localiser les conduits de services publics de grands diam\u00e8tres et les infrastructures abandonn\u00e9es de mines tels que galeries, chambres, canalisations d'air et puits.<\/p>\n<p>\u00a0<\/p>\n<p>\u00a0<\/p>\n<p>Pour plus d'information, veuillez contacter notre <a href=\"mailto:daniel.campos@geophysicsgpr.com;jean-luc.arsenault@geophysicsgpr.com;claude.robillard@geophysicsgpr.com;info@geophysicsgpr.com\">\u00c9quipe de Lev\u00e9 Terrestre<\/a>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-874-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-874-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-874-1-0-0\" 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-874-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-874\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Applications_Subsidence_cavities_3.jpg\" width=\"563\" height=\"174\" srcset=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Applications_Subsidence_cavities_3.jpg 563w, https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Applications_Subsidence_cavities_3-300x93.jpg 300w\" sizes=\"auto, (max-width: 563px) 100vw, 563px\" title=\"Ground Applications Subsidence cavities\" alt=\"Cartographie des vides\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-874-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-874-1-1-0\" 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-874-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-874\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_ResIP_Exploration.jpg\" width=\"155\" height=\"191\" sizes=\"auto, (max-width: 155px) 100vw, 155px\" title=\"Ground Techniques ResIP Exploration\" alt=\"Cartographie des vides\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Exemples d&rsquo;applications classiques de la cartographie des videsLa cartographie des vides est une m\u00e9thode \u00e9lectrique de la g\u00e9ophysique terrestre appliqu\u00e9e \u00e0 la quantification des volumes de terrains, les intrusions min\u00e9rales et \u00e0 la cartographie des r\u00e9sistivit\u00e9s apparentes.Les m\u00e9thodes g\u00e9ophysiques permettent d&rsquo;identifier et de cartographier efficacement les zones d&rsquo;affaissement de sols, les vides, les cavit\u00e9s et&#8230;  <a href=\"https:\/\/ground.geophysicsgpr.com\/fr\/techniques-de-geophysique-terrestre\/resistivite-electrique-pp-ps\/cartographie-des-vides\" class=\"more-link\" title=\"Read Cartographie des vides\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":1118,"parent":846,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-874","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/874","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/comments?post=874"}],"version-history":[{"count":1,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/874\/revisions"}],"predecessor-version":[{"id":3020,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/874\/revisions\/3020"}],"up":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/846"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media\/1118"}],"wp:attachment":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/media?parent=874"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}