{"id":1017,"date":"2015-07-21T16:58:02","date_gmt":"2015-07-21T16:58:02","guid":{"rendered":"http:\/\/ground.geophysicsgpr.com\/?page_id=1017"},"modified":"2015-11-14T01:27:17","modified_gmt":"2015-11-14T01:27:17","slug":"etudes-hydrogeologiques","status":"publish","type":"page","link":"https:\/\/ground.geophysicsgpr.com\/fr\/applications-geophysique-terrestre\/etudes-hydrogeologiques","title":{"rendered":"\u00c9tudes hydrog\u00e9ologiques"},"content":{"rendered":"<div id=\"pl-1017\"  class=\"panel-layout\" ><div id=\"pg-1017-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-1017-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-1017-0-0-0\" 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-1017-0-0-0\" ><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 techniques g\u00e9ophysiques peuvent fournir des informations cl\u00e9s aux \u00e9tudes hydrog\u00e9ologiques permettant ainsi un forage mieux cibl\u00e9.\u00a0<\/p>\n<p>G\u00e9ophysique GPR a utilis\u00e9 la sismique pour identifier des pal\u00e9ochenaux et des zones de fracturation menant \u00e0 l'identification d'aquif\u00e8res sur de nombreux sites \u00e9tudi\u00e9s. Les m\u00e9thodes \u00e9lectriques peuvent servir pour cartographier l'\u00e9tendue des aquif\u00e8res en trois dimensions.\u00a0<\/p>\n<p>Une fois le puits for\u00e9, l'exp\u00e9rience de G\u00e9ophysique GPR en diagraphie peut optimiser la conception du cr\u00e9pinage du puits.<\/p>\n<p>\u00a0<br \/> Les essais hydrog\u00e9ologiques servent \u00e0 documenter le comportement hydraulique des aquif\u00e8res.<\/p>\n<h2 class=\"h2resize\">Avec les \u00e9tudes hydrog\u00e9ologiques, la caract\u00e9risation des aquif\u00e8res inclut, sans s\u2019y limiter les points suivants :<\/h2>\n<ul>\n<li>D\u00e9terminer la conductivit\u00e9 hydraulique \u00e0 proximit\u00e9 d\u2019un pi\u00e9zom\u00e8tre;<\/li>\n<li>D\u00e9terminer les propri\u00e9t\u00e9s hydrog\u00e9ologiques d\u2019un aquif\u00e8re telles la transmissivit\u00e9, et le coefficient d\u2019emmagasinement, etc.;<\/li>\n<li>D\u00e9terminer la capacit\u00e9 de pompage d\u2019un puits;<\/li>\n<li>V\u00e9rifier la performance de la construction d\u2019un puits;<\/li>\n<li>D\u00e9terminer la direction et la vitesse d\u2019\u00e9coulement des eaux souterraines.<\/li>\n<\/ul>\n<p>\u00a0<\/p>\n<p>Pour plus d'information, veuillez contacter notre <a href=\"mailto:daniel.campos@gprmtl.com;jean-luc.arsenault@gprmtl.com;claude.robillard@gprmtl.com;info@gprmtl.com\">\u00c9quipe de Lev\u00e9 Terrestre<\/a>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pgc-1017-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-1017-0-1-0\" 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-1017-0-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-1017\"\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_Hydrogeology_2-Custom.jpg\" width=\"188\" height=\"250\" sizes=\"auto, (max-width: 188px) 100vw, 188px\" title=\"Ground Applications Hydrogeology\" alt=\"\u00e9tudes hydrog\u00e9ologiques\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-1017-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-1017-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-1017-1-0-0\" 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-1017-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-1017\"\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_Hydrogeology_3-Custom.png\" width=\"640\" height=\"238\" srcset=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Applications_Hydrogeology_3-Custom.png 640w, https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Applications_Hydrogeology_3-Custom-300x112.png 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" title=\"Ground Applications Hydrogeology\" alt=\"\u00e9tudes hydrog\u00e9ologiques\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-1017-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-1017-1-1-0\" 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-1017-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-1017\"\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_resistivity_Ground-water.jpg\" width=\"640\" height=\"254\" srcset=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_resistivity_Ground-water.jpg 640w, https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_resistivity_Ground-water-300x119.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" title=\"Ground Techniques resistivity Ground water\" alt=\"Ground Techniques resistivity Ground water\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Les techniques g\u00e9ophysiques peuvent fournir des informations cl\u00e9s aux \u00e9tudes hydrog\u00e9ologiques permettant ainsi un forage mieux cibl\u00e9.\u00a0G\u00e9ophysique GPR a utilis\u00e9 la sismique pour identifier des pal\u00e9ochenaux et des zones de fracturation menant \u00e0 l&rsquo;identification d&rsquo;aquif\u00e8res sur de nombreux sites \u00e9tudi\u00e9s. Les m\u00e9thodes \u00e9lectriques peuvent servir pour cartographier l&rsquo;\u00e9tendue des aquif\u00e8res en trois dimensions.\u00a0Une fois le&#8230;  <a href=\"https:\/\/ground.geophysicsgpr.com\/fr\/applications-geophysique-terrestre\/etudes-hydrogeologiques\" class=\"more-link\" title=\"Read \u00c9tudes hydrog\u00e9ologiques\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":1118,"parent":707,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-1017","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/1017","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=1017"}],"version-history":[{"count":0,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/1017\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/fr\/wp-json\/wp\/v2\/pages\/707"}],"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=1017"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}