{"id":4804,"date":"2020-04-11T23:47:54","date_gmt":"2020-04-11T21:47:54","guid":{"rendered":"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/?page_id=4804"},"modified":"2020-12-05T00:52:20","modified_gmt":"2020-12-04T23:52:20","slug":"olivier-morio-these","status":"publish","type":"page","link":"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/en\/theses-post-docs\/olivier-morio-these\/","title":{"rendered":"Olivier Morio (PhD)"},"content":{"rendered":"<div id=\"pl-4804\"  class=\"panel-layout\" ><div id=\"pg-4804-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4804-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4804-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div class=\"panel-widget-style panel-widget-style-for-4804-0-0-0\" ><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 style=\"text-align: left;\"><span style=\"color: #ffffff;\"><img loading=\"lazy\" decoding=\"async\" class=\"alignleft wp-image-4723\" src=\"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/Olivier-Morio.jpg\" alt=\"\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/Olivier-Morio.jpg 189w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/Olivier-Morio-150x150.jpg 150w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/span><\/p>\n<h3 style=\"text-align: center;\"><span style=\"color: #ffffff;\">Olivier Morio<\/span><\/h3>\n<p>&nbsp;<\/p>\n<p style=\"text-align: left;\">Thesis defended on December 20th 2017<\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div><div id=\"pg-4804-1\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4804-1-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4804-1-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"1\" ><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<h3 style=\"text-align: center;\">Understanding the morpho-sedimentary dynamics of cohesive and non- cohesive beaches in the South-Brittany region (France) at different spatiotemporal scales<\/h3>\n<\/div>\n<\/div><\/div><\/div><\/div><div id=\"pg-4804-2\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-4804-2-0\"  class=\"panel-grid-cell\" ><div id=\"panel-4804-2-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"2\" ><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<h4 style=\"text-align: left;\"><span style=\"color: #1269b0;\">Abstract<\/span><\/h4>\n<p style=\"text-align: justify;\"><span style=\"color: #4b4b4c;\">At the world scale, coastal areas can be divided in several categories: rocky, sandy muddy and\nmixed coasts. However, these sedimentary coasts are regularly found mixed. Temporary or\npermanent mud inputs are observed on the sandy beaches. These atypical mixed environments,\ncoupling erosional, transports and deposits processes associated to cohesive and non-cohesive\nsediments have been poorly studied. So, understanding theirs morphological and sedimentary\ndynamics and the identification of regional and local forcings driving them are essential.\nFour sandy-muddy or fully sandy Low-Tide-Terrace beaches from the bay and estuary of Vilaine\n(South-Brittany) have been monthly monitored over two years to characterize their morphodynamics\nbeahaviors. Specific monitoring of coupled hydrodynamics and morpho-sedimentary surveys and\nphotogrammetry experiments have been conducted on mixed sandy-muddy or full sandy beaches.\nAt a regional scale, this work highlights the role of the initial morphology and regional geology\ninheritance on the morphological response of the littoral zones to extreme energy conditions.\nDespite some erosion patterns in local parts of beaches, particularly close to shore protection\nstructures, the mid-term recovery capacity of the south-Brittany coastal area after extreme wave\nenergy conditions have been proved. In a more specific approach, the works regarding the sandymuddy beach dynamic show a morphodynamics behaviour close to that of a fully sandy beach during\nhigh energy event. The mudflat elevation changes and the dynamic of the ridges and runnels\nsedimentary patterns are mainly controlled by the incoming waves but also by the own physical\nproperties of the sediment, particularly those induced by the interaction between the sand from the\nreflective section and the mudflat. A sand deposit between mud layers potentially decreases the\nwave erosion capacity on the mudflat.<\/span><\/p>\n<\/div>\n<\/div><\/div><\/div><div id=\"pgc-4804-2-1\"  class=\"panel-grid-cell\" ><div id=\"panel-4804-2-1-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"3\" ><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<h4 style=\"padding-left: 40px;\"><a href=\"https:\/\/tel.archives-ouvertes.fr\/tel-01922745\/document\" target=\"_blank\" rel=\"noopener\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-4805\" src=\"http:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/icons8-document-500_blue-1-300x300.png\" alt=\"\" width=\"100\" height=\"100\" srcset=\"https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/icons8-document-500_blue-1-300x300.png 300w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/icons8-document-500_blue-1-150x150.png 150w, https:\/\/www.laboratoire-geosciences-ocean-ubs.fr\/wp-content\/uploads\/2020\/04\/icons8-document-500_blue-1.png 500w\" sizes=\"auto, (max-width: 100px) 100vw, 100px\" \/><\/a><\/h4>\n<p style=\"text-align: left; padding-left: 40px;\"><span style=\"color: #1269b0;\"><strong>Supervisors<\/strong><br \/>\n<\/span><span style=\"color: #4b4b4c;\">Evelyne Goubert<br \/>\nMouncef Sedrati<\/span><\/p>\n<p style=\"padding-left: 40px;\"><strong><span style=\"color: #1269b0;\">Members of the jury<br \/>\n<\/span><\/strong><span style=\"color: #4b4b4c;\">Paul Fattal<\/span><br \/>\n<span style=\"color: #4b4b4c;\">Franck Dolique<\/span><\/p>\n<p style=\"padding-left: 40px;\"><strong><span style=\"color: #1269b0;\">Rapporteurs<\/span><\/strong><br \/>\n<span style=\"color: #4b4b4c;\">Herv\u00e9 Regnauld<\/span><br \/>\n<span style=\"color: #4b4b4c;\">Antoine Gardel<\/span><\/p>\n<p style=\"text-align: left; padding-left: 40px;\"><strong><span style=\"color: #1269b0;\">Keywords<br \/>\n<\/span><\/strong><span style=\"color: #4b4b4c;\">Mud<br \/>\nSand<br \/>\nLittorals<br \/>\nModifications<br \/>\nStorms effects<br \/>\nFrance<br \/>\nVilaine estuary<\/span><\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Olivier Morio &nbsp; Th\u00e8se soutenue le 20-12-2017 Compr\u00e9hension des dynamiques morpho-s\u00e9dimentaires coh\u00e9sives et non- coh\u00e9sives des littoraux de Bretagne Sud (France) \u00e0 diff\u00e9rentes \u00e9chelles spatio- temporelles<\/p>","protected":false},"author":9,"featured_media":5142,"parent":3951,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-4804","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - 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