{"id":238,"date":"2015-08-06T15:29:13","date_gmt":"2015-08-06T14:29:13","guid":{"rendered":"http:\/\/marine.geophysicsgpr.com\/?page_id=238"},"modified":"2017-03-10T19:53:49","modified_gmt":"2017-03-10T18:53:49","slug":"sedimentation-study","status":"publish","type":"page","link":"https:\/\/marine.geophysicsgpr.com\/en\/marine-geophysics-applications\/geological-and-geotechnical\/sedimentation-study","title":{"rendered":"Sedimentation Studies"},"content":{"rendered":"<div id=\"pl-238\"  class=\"panel-layout\" ><div id=\"pg-238-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-238-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-238-0-0-0\" 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-238-0-0-0\" ><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>A basic sedimentation study implies high precision bathymetric surveys repeated over a fixed time interval. Using this information, estimates can be made on the rate of sedimentation in navigation channels, upstream of dam intakes, in ports or marinas etc. A more detailed study would include additional types of measurements.<\/p>\n<h2 class=\"h2resize\">A typical sedimentation study may include the following :<\/h2>\n<p>High precision bathymetric surveys;<br \/> Side-scan sonar surveys;<br \/> Marine geological profiling in critical areas;<br \/> Water and sediment sampling;<br \/> Tide and current measurements.<\/p>\n<p>\u00a0<\/p>\n<p>For more information, please contact our <span style=\"color: #317671\"><a href=\"mailto:info@geophysicsgpr.com\">Marine Survey Team<\/a><\/span>.<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-238-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-238-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-238-1-0-0\" 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-238-1-0-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-238\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_Sediment-Thickness.jpg\" width=\"640\" height=\"467\" srcset=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_Sediment-Thickness.jpg 640w, https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/Marine_applications_Sediment-Thickness-300x219.jpg 300w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" title=\"Marine_applications_Sediment Thickness\" alt=\"Sedimentation study\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><div id=\"pgc-238-1-1\"  class=\"panel-grid-cell\" ><div id=\"panel-238-1-1-0\" 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-238-1-1-0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-image so-widget-sow-image-default-8b5b6f678277-238\"\n\t\t\t\n\t\t>\n<div class=\"sow-image-container\">\n\t\t<img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/marine.geophysicsgpr.com\/wp-content\/uploads\/sites\/5\/2015\/07\/marine_applications_environment_sediment_inset.jpg\" width=\"163\" height=\"180\" sizes=\"auto, (max-width: 163px) 100vw, 163px\" title=\"marine_applications_environment_sediment_inset\" alt=\"Sedimentation study\" \t\tclass=\"so-widget-image\"\/>\n\t<\/div>\n\n<\/div><\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>A basic sedimentation study implies high precision bathymetric surveys repeated over a fixed time interval. Using this information, estimates can be made on the rate of sedimentation in navigation channels, upstream of dam intakes, in ports or marinas etc. A more detailed study would include additional types of measurements.A typical sedimentation study may include the&#8230;  <a href=\"https:\/\/marine.geophysicsgpr.com\/en\/marine-geophysics-applications\/geological-and-geotechnical\/sedimentation-study\" class=\"more-link\" title=\"Read Sedimentation Studies\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":1,"featured_media":78,"parent":176,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-full-width.php","meta":{"content-type":"","footnotes":""},"class_list":["post-238","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/238","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/comments?post=238"}],"version-history":[{"count":14,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/238\/revisions"}],"predecessor-version":[{"id":1664,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/238\/revisions\/1664"}],"up":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/pages\/176"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media\/78"}],"wp:attachment":[{"href":"https:\/\/marine.geophysicsgpr.com\/en\/wp-json\/wp\/v2\/media?parent=238"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}