{"id":1015,"date":"2015-07-21T16:58:02","date_gmt":"2015-07-21T16:58:02","guid":{"rendered":"http:\/\/ground.geophysicsgpr.com\/?page_id=1015"},"modified":"2017-03-10T19:37:41","modified_gmt":"2017-03-10T19:37:41","slug":"hydrogeological-studies","status":"publish","type":"page","link":"https:\/\/ground.geophysicsgpr.com\/en\/ground-geophysics-applications\/hydrogeological-studies","title":{"rendered":"Hydrogeological Studies"},"content":{"rendered":"<div id=\"pl-1015\"  class=\"panel-layout\" ><div id=\"pg-1015-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-1015-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-1015-0-0-0\" 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-1015-0-0-0\" ><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>Geophysical techniques can provide key insights to hydrogeological studies allowing for focused drilling. Geophysics GPR has employed seismic surveys to identified bedrock paleochannels and fracture zones leading to successful water sources at numerous sites. Electrical methods can be used for mapping the 3D extents of aquifers.<\/p>\n<p>Once drilled, Geophysics GPR's experience in borehole logging can optimize the screening and well design.<\/p>\n<p>\u00a0<\/p>\n<p>For more information, please contact our\u00a0<a href=\"mailto:info@geophysicsgpr.com\">Ground Survey Team<\/a>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pgc-1015-0-1\"  class=\"panel-grid-cell\" ><div id=\"panel-1015-0-1-0\" 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-1015-0-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-1015\"\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=\"Hydrogeological Studies\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-1015-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-1015-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-1015-1-0-0\" 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-1015-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-1015\"\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=\"Ground Applications Hydrogeology\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-1015-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-1015-1-1-0\" 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-1015-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-1015\"\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=\"Hydrogeological Studies\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Geophysical techniques can provide key insights to hydrogeological studies allowing for focused drilling. Geophysics GPR has employed seismic surveys to identified bedrock paleochannels and fracture zones leading to successful water sources at numerous sites. Electrical methods can be used for mapping the 3D extents of aquifers.Once drilled, Geophysics GPR&#8217;s experience in borehole logging can optimize&#8230;  <a href=\"https:\/\/ground.geophysicsgpr.com\/en\/ground-geophysics-applications\/hydrogeological-studies\" class=\"more-link\" title=\"Read Hydrogeological Studies\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":1118,"parent":705,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-1015","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/1015","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/comments?post=1015"}],"version-history":[{"count":3,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/1015\/revisions"}],"predecessor-version":[{"id":3070,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/1015\/revisions\/3070"}],"up":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/705"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media\/1118"}],"wp:attachment":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media?parent=1015"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}