{"id":858,"date":"2015-07-21T16:15:58","date_gmt":"2015-07-21T16:15:58","guid":{"rendered":"http:\/\/ground.geophysicsgpr.com\/?page_id=858"},"modified":"2017-03-10T19:20:23","modified_gmt":"2017-03-10T19:20:23","slug":"hydrogeology","status":"publish","type":"page","link":"https:\/\/ground.geophysicsgpr.com\/en\/techniques\/electrical-resistivity-ip-and-sp\/hydrogeology","title":{"rendered":"Hydrogeology"},"content":{"rendered":"<div id=\"pl-858\"  class=\"panel-layout\" ><div id=\"pg-858-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-858-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-858-0-0-0\" 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-858-0-0-0\" ><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>Hydrogeology deals with the distribution and movement of groundwater in the soil and rocks. \u00a0Electrical resistivity surveys are used for\u00a0generating sub-surface models for hydrogeologicial studies and can play a critical role in optimizing drilling.<\/p>\n<p>The method of spontaneous potential (SP) can be used to study the flow of water in the soil.<\/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><div id=\"pg-858-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-858-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-858-1-0-0\" 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-858-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-858\"\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_water.jpg\" width=\"640\" height=\"323\" srcset=\"https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_Resistivity_water.jpg 640w, https:\/\/ground.geophysicsgpr.com\/wp-content\/uploads\/sites\/7\/2015\/07\/Ground_Techniques_Resistivity_water-300x151.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" title=\"Ground Techniques Resistivity ground water\" alt=\"Hydrogeology - Ground Geophysics\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-858-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-858-1-1-0\" 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-858-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-858\"\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=\"160\" height=\"213\" sizes=\"auto, (max-width: 160px) 100vw, 160px\" title=\"Ground Techniques Resistivity ground water\" alt=\"Hydrogeology - Ground Geophysics\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Hydrogeology deals with the distribution and movement of groundwater in the soil and rocks. \u00a0Electrical resistivity surveys are used for\u00a0generating sub-surface models for hydrogeologicial studies and can play a critical role in optimizing drilling.The method of spontaneous potential (SP) can be used to study the flow of water in the soil.For more information, please contact&#8230;  <a href=\"https:\/\/ground.geophysicsgpr.com\/en\/techniques\/electrical-resistivity-ip-and-sp\/hydrogeology\" class=\"more-link\" title=\"Read Hydrogeology\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":1118,"parent":844,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-858","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/858","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=858"}],"version-history":[{"count":2,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/858\/revisions"}],"predecessor-version":[{"id":3051,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/858\/revisions\/3051"}],"up":[{"embeddable":true,"href":"https:\/\/ground.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/844"}],"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=858"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}