{"id":133380,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/geomorfologia-y-evolucion-de-la-red-de-desague-de-una-cuenca-interpretacion-y-comportamiento\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"geomorfologia-y-evolucion-de-la-red-de-desague-de-una-cuenca-interpretacion-y-comportamiento","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geomorfologia-y-evolucion-de-la-red-de-desague-de-una-cuenca-interpretacion-y-comportamiento\/","title":{"rendered":"Geomorfolog\u00eda y evolucion de la red de desague de una cuenca. interpretacion y comportamiento."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Adolfo Pe\u00f1a Acevedo <\/strong><\/h2>\n<p>El hidrograma unitario instantaneo geomorfologico, huig, desarrollado en este trabajo, permite obtener la respuesta unitaria de la cuenca, y es sensible a la disposicion topologica de los canales en la red de desague. El uso de funciones de distribucion exponenciales para los tiempos de espera en los canales y en las laderas con velocidades de viaje de distinto orden de magnitud, permite observar la analogia entre la cuenca y su representacion como un conjunto embalses lineales en serie y en paralelo. La extraccion de redes de desague a partir de datos digitales de elevacion, ha permitido cuantificar geomorfologicamente la estructura topologica de los canales en cuencas reales. Se han desarrollado algoritmos propios para el analisis digital de la cuenca, presentandose un procedimiento eficaz para obtener la divisoria de la cuenca a partir de su modelo digital de elevacion, mde, basado en el recorrido en arbol de los patrones de flujo. Se ha incorporado el calculo de magnitudes geomorfologicas asociadas a cada tramo de canal, procediendose por ordenes, cuando la red es clasificada siguiendo el criterio de strahler.  finalmente, se han aplicado los procedimientos descritos a una cuenca de alta monta\u00f1a del sureste espa\u00f1ol, obteniendose resultados satisfactorios en la cuantificacion geomorfologica de la red de desague a partir de datos digitales y diversos huig, que se muestra como un instrumento util para obtener la respuesta de cuencas fluviales a aguaceros.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Geomorfolog\u00eda y evolucion de la red de desague de una cuenca. interpretacion y comportamiento.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Geomorfolog\u00eda y evolucion de la red de desague de una cuenca. interpretacion y comportamiento. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Adolfo Pe\u00f1a Acevedo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 C\u00f3rdoba<\/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>Jos\u00e9 Luis Ayuso Mu\u00f1oz<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Rold\u00e1n Ca\u00f1as <\/li>\n<li>Joaqu\u00edn Andreu \u00e1lvarez (vocal)<\/li>\n<li>Fernando Ca\u00f1izal Berini (vocal)<\/li>\n<li>Ana Mar\u00eda Laguna Luna (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Adolfo Pe\u00f1a Acevedo El hidrograma unitario instantaneo geomorfologico, huig, desarrollado en este trabajo, permite obtener la respuesta [&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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