{"id":14355,"date":"2001-11-12T00:00:00","date_gmt":"2001-11-12T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/balana%c2%a7-de-sediment-i-dinamica-fluvial-en-un-system-de-regim-hidrhologic-tramsitori-tram-final-de-la-tordera\/"},"modified":"2001-11-12T00:00:00","modified_gmt":"2001-11-12T00:00:00","slug":"balana%c2%a7-de-sediment-i-dinamica-fluvial-en-un-system-de-regim-hidrhologic-tramsitori-tram-final-de-la-tordera","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/balana%c2%a7-de-sediment-i-dinamica-fluvial-en-un-system-de-regim-hidrhologic-tramsitori-tram-final-de-la-tordera\/","title":{"rendered":"Balan\u00c1\u00a7 de sediment i din\u00e1mica fluvial en un system de regim hidrhologic tramsitori (tram final de la tordera)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Alberto Rovira Garcia <\/strong><\/h2>\n<p>El balance de sedimento del tramo un feria de la tordera est\u00e1 directamente controlado por la bimodalidad hidrol\u00f3gica del r\u00edo, y por el n\u00famero y la magnitud de las crecidas que ocurren en la entrada y salida del sistema. en el recto inicial.  el 75% del sedimento es transportado durante crecidas iguales o inferiores al canal lleno, mientras que al final 10 de m\u00e1s del 90%. El tr\u00e1nsito anual medio de sedimento ha sido de 30.000 toneladas (60% como sedimento de fondo y 40% den suspensi\u00f3n) en la entrada del sistema, y de 21.500 toneladas (65% como carga de fondo y el 35% en suspensi\u00f3n y a la salida, con una acumulaci\u00f3n media anual en el canal de 8.500 toneladas).<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Balan\u00c1\u00a7 de sediment i din\u00e1mica fluvial en un system de regim hidrhologic tramsitori (tram final de la tordera)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Balan\u00c1\u00a7 de sediment i din\u00e1mica fluvial en un system de regim hidrhologic tramsitori (tram final de la tordera) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Alberto Rovira Garcia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 11\/12\/2001<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Mar\u00eda Sala Sanjaume<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: josep m. Panareda i clop\u00e9s <\/li>\n<li>Jorge Guill\u00e9n aranda (vocal)<\/li>\n<li>jordi Serra raventos (vocal)<\/li>\n<li>Francisco Segura beltran (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alberto Rovira Garcia El balance de sedimento del tramo un feria de la tordera est\u00e1 directamente controlado [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[16509,951,27,5742,17708,1666],"tags":[46249,46250,15841,37405,28365,34205],"class_list":["post-14355","post","type-post","status-publish","format-standard","hentry","category-aguas-superficiales","category-barcelona","category-ciencias-de-la-tierra-y-del-espacio","category-ciencias-geograficas","category-geografia-de-los-recursos-naturales","category-hidrologia","tag-alberto-rovira-garcia","tag-francisco-segura-beltran","tag-jordi-serra-raventos","tag-jorge-guillen-aranda","tag-josep-m-panareda-i-clopes","tag-maria-sala-sanjaume"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/14355","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=14355"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/14355\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=14355"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=14355"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=14355"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}