{"id":910,"date":"2015-07-21T16:27:15","date_gmt":"2015-07-21T16:27:15","guid":{"rendered":"http:\/\/ground.geophysicsgpr.com\/?page_id=910"},"modified":"2017-03-02T16:02:31","modified_gmt":"2017-03-02T16:02:31","slug":"profilage-des-sols-et-du-roc","status":"publish","type":"page","link":"https:\/\/ground.geophysicsgpr.com\/fr\/applications-geophysique-terrestre\/etudes-geologiques-et-geotechniques\/profilage-des-sols-et-du-roc","title":{"rendered":"Profilage des sols et du roc"},"content":{"rendered":"<div id=\"pl-910\"  class=\"panel-layout\" ><div id=\"pg-910-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-910-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-910-0-0-0\" 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-910-0-0-0\" ><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>G\u00e9ophysique GPR dispose d'une grande exp\u00e9rience dans la cartographie des d\u00e9p\u00f4ts meubles et du roc ainsi que dans l'identification, parmi les nombreuses techniques g\u00e9ophysiques disponibles, de celles qui r\u00e9pondront le mieux selon le contexte.<\/p>\n<p>Ces choix doivent r\u00e9pondre \u00e0 plusieurs imp\u00e9ratifs dont prioritairement, l'information recherch\u00e9e par le client, mais aussi les conditions environnementales et g\u00e9ologiques du site \u00e0 l'\u00e9tude et les principes g\u00e9ophysiques sur lesquels s'appuient chaque m\u00e9thode d'investigation.<\/p>\n<h2 class=\"h2resize\">Diff\u00e9rentes m\u00e9thodes pour le profilage des sols et du roc.<\/h2>\n<p>Les m\u00e9thodes sismiques, qu'elles soient de r\u00e9fraction, r\u00e9flexion, r\u00e9sonance ou d'analyse d'ondes de surface, sont les techniques les plus reconnues pour cartographier et identifier les caract\u00e9ristiques du substrat rocheux sous un vaste \u00e9ventail de conditions de terrain. Lorsque l'objectif consiste \u00e0 cartographier la profondeur du roc sain dans le cadre de projets d'ing\u00e9nierie, c'est la sismique r\u00e9fraction qui s'av\u00e8re l'option \u00e0 retenir.<\/p>\n<p>Les lev\u00e9s de r\u00e9sistivit\u00e9 \u00e9lectrique et la tomographie PP sont id\u00e9als pour des investigations environnementales et hydrog\u00e9ologiques pour d\u00e9terminer les propri\u00e9t\u00e9s du sol, la dispersion des contaminants ou l'\u00e9tude des eaux souterraines.<\/p>\n<p>D'autres m\u00e9thodes, incluant la gravim\u00e9trie, le g\u00e9oradar et d'autres techniques \u00e9lectromagn\u00e9tiques sont aussi r\u00e9guli\u00e8rement employ\u00e9es pour cartographier la g\u00e9ologie.<\/p>\n<p>Les sections consacr\u00e9es aux m\u00e9thodes a\u00e9roport\u00e9es et marines de notre site pr\u00e9sentent respectivement les services offerts de cartographie a\u00e9rienne et sous-marine.<\/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 id=\"pgc-910-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-910-0-1-0\" class=\"so-panel widget widget_sow-image panel-first-child\" data-index=\"1\" ><div class=\"panel-widget-style panel-widget-style-for-910-0-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-910\"\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_Geotech_Overburden-and-Bedrock_4-Custom.jpg\" width=\"225\" height=\"169\" sizes=\"auto, (max-width: 225px) 100vw, 225px\" title=\"Ground technique Profilage des sols et du roc\" alt=\"Profilage des sols et du roc\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><div id=\"panel-910-0-1-1\" class=\"so-panel widget widget_sow-image panel-last-child\" data-index=\"2\" ><div class=\"panel-widget-style panel-widget-style-for-910-0-1-1\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-910\"\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_Geotech_Overburden-and-Bedrock_2-Custom.jpg\" width=\"225\" height=\"300\" sizes=\"auto, (max-width: 225px) 100vw, 225px\" title=\"Ground technique Profilage des sols et du roc\" alt=\"Profilage des sols et du roc\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-910-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-910-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-910-1-0-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"3\" ><div class=\"panel-widget-style panel-widget-style-for-910-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-910\"\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_overburden_seismic.png\" width=\"589\" height=\"277\" srcset=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_applications_overburden_seismic.png 589w, https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_applications_overburden_seismic-300x141.png 300w\" sizes=\"auto, (max-width: 589px) 100vw, 589px\" title=\"Ground technique Profilage des sols et du roc\" alt=\"Profilage des sols et du roc\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-910-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-910-1-1-0\" class=\"so-panel widget widget_sow-image panel-first-child panel-last-child\" data-index=\"4\" ><div class=\"panel-widget-style panel-widget-style-for-910-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-910\"\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_Geotech_Overburden-and-Bedrock_3-e1446832090624.jpg\" width=\"687\" height=\"449\" srcset=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Applications_Geotech_Overburden-and-Bedrock_3-e1446832090624.jpg 687w, https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Applications_Geotech_Overburden-and-Bedrock_3-e1446832090624-300x196.jpg 300w\" sizes=\"auto, (max-width: 687px) 100vw, 687px\" title=\"Ground technique Profilage des sols et du roc\" alt=\"Profilage des sols et du roc\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>G\u00e9ophysique GPR dispose d&rsquo;une grande exp\u00e9rience dans la cartographie des d\u00e9p\u00f4ts meubles et du roc ainsi que dans l&rsquo;identification, parmi les nombreuses techniques g\u00e9ophysiques disponibles, de celles qui r\u00e9pondront le mieux selon le contexte.Ces choix doivent r\u00e9pondre \u00e0 plusieurs imp\u00e9ratifs dont prioritairement, l&rsquo;information recherch\u00e9e par le client, mais aussi les conditions environnementales et g\u00e9ologiques du&#8230;  <a href=\"https:\/\/ground.geophysicsgpr.com\/fr\/applications-geophysique-terrestre\/etudes-geologiques-et-geotechniques\/profilage-des-sols-et-du-roc\" class=\"more-link\" title=\"Read Profilage des sols et du roc\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":1118,"parent":903,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-910","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/910","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=910"}],"version-history":[{"count":1,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/910\/revisions"}],"predecessor-version":[{"id":3031,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/910\/revisions\/3031"}],"up":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/903"}],"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=910"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}