{"id":133032,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/transporte-de-fondo-en-un-rio-de-gravas-y-su-relacion-con-la-dinamica-del-lecho-fluvial\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"transporte-de-fondo-en-un-rio-de-gravas-y-su-relacion-con-la-dinamica-del-lecho-fluvial","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/transporte-de-fondo-en-un-rio-de-gravas-y-su-relacion-con-la-dinamica-del-lecho-fluvial\/","title":{"rendered":"Transporte de fondo en un rio de gravas y su relacion con la dinamica del lecho fluvial."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Celso Garcia Garcia <\/strong><\/h2>\n<p>Durante dos a\u00f1os el transporte de fondo ha sido medido en un rio con lecho de gravas: el tordera. Para medir las tasas de transporte de fondo se ha utilizado un sistema automatico, denominado de presion en un cojin, que permite la medida continua del transporte. Al mismo tiempo, las formas del lecho fluvial han sido descritas mediante el uso de la fotografia vertical, agrupandolas por tama\u00f1os del sedimento y localizandolas en el cauce mediante un sistema de coordenadas.  los resultados han corroborado la gran variabilidad temporal y espacial del transporte de fondo durante las crecidas. La principal fuente de sedimento durante el inicio del transporte son las formas de material fino del lecho: los parches. A medida que los parches desaparecen, debido a la falta de sedimento, la fuente de sedimento es la subsuperficie del lecho, una vez que la coraza superficial se ha roto parcialmente.  la disponibilidad del sedimento, en forma de agrupaciones en el lecho, es la principal causa de las variaciones en las tasas del transporte de fondo en un rio de gravas de monta\u00f1a media mediterranea. Esta variabilidad dificulta la prediccion del transporte de fondo mediante el uso de una ecuacion y la deduccion de una curva empirica para el rio tordera.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Transporte de fondo en un rio de gravas y su relacion con la dinamica del lecho fluvial.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Transporte de fondo en un rio de gravas y su relacion con la dinamica del lecho fluvial. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Celso Garcia Garcia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/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: Antonio Gomez Ortiz <\/li>\n<li>Juan  Pedro Mart\u00edn Vide (vocal)<\/li>\n<li>Gerardo Benito Ferrandez (vocal)<\/li>\n<li>Francisca Segura Beltran (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Celso Garcia Garcia Durante dos a\u00f1os el transporte de fondo ha sido medido en un rio con [&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 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