{"id":14079,"date":"2018-03-09T09:00:38","date_gmt":"2018-03-09T09:00:38","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/geomorfologia-e-hidrologia-fluvial-del-rio-alberche-modelos-y-s-i-g-para-la-gestion-de-riberas\/"},"modified":"2018-03-09T09:00:38","modified_gmt":"2018-03-09T09:00:38","slug":"geomorfologia-e-hidrologia-fluvial-del-rio-alberche-modelos-y-s-i-g-para-la-gestion-de-riberas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geomorfologia-e-hidrologia-fluvial-del-rio-alberche-modelos-y-s-i-g-para-la-gestion-de-riberas\/","title":{"rendered":"Geomorfolog\u00eda e hidrolog\u00eda fluvial del rio alberche: modelos y s.i.g. para la gestion de riberas"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Andres Diez Herrero <\/strong><\/h2>\n<p>Mediante tecnicas de an\u00e1lisis hidrol\u00f3gico y geomorfol\u00f3gico, y el empleo de herramientas matematicas e inform\u00e1ticas (sistemas de informacion geografica) se ha conseguido modelizar la respuesta de un sistema fluvial(rio alberche, tributario del rio tajo por su margen derecha) ante eventos hidrol\u00f3gicos extremos (crecidas y avenidas) y predecir cuantitativamente las conecuencias de las intervenciones antr\u00f3picas en su cauce y la cuenca que drena.  para ello, ha sido preciso el uso combinado e integrado de diversas metodolog\u00edas: tecnicas de gabinete, como recopilacion de informaci\u00f3n, cartograf\u00eda geomorfol\u00f3gica desde fotointerpretaci\u00f3n estereoscopica, analisis estadistico de datos numericos, aplicaci\u00f3n de modelos matematicos hidrol\u00f3gicos e hidr\u00e1ulicos, desarrollo de un sistema de informaci\u00f3n geogr\u00e1fica, estudio morfodin\u00e1mico de meandros fluviales y an\u00e1lisis meteorol\u00f3gico de im\u00e1genes de teledetecci\u00f3n radar; tecnicas de laboratorio, comprendiendo analisis mineral\u00f3gicos y granulom\u00e9tricos, dataci\u00f3n de muestras por luminiscencia y radiocarbono, y estudios paleopalinol\u00f3gicos; y tecnicas de campo, desde mediciones morfom\u00e9tricas e hidrologicas, a la revision de la cartografia geomorfologica, pasando por la toma de muestras, adquisicion de documentos graficos y levantamiento de columnas y perfiles.  entre los resultados obtenidos destacan: una nueva cartografia geomorfologica de la cuenca a escala 1:50.000; un modelo de evolucion cuaternaria de la red de drenaje del rio alberche; un esquema de la configuracion e interpretacion gen\u00e9tica de los sistemas de terrazas y llanuras aluviales de la cuenca; la caracterizacion hidrol\u00f3gica de las corrientes fluviales, incluyendo calculos hidrometeorol\u00f3gicos, analisis estadisticos y estudios paleohidrologicos de crecidas y avenidas(ordinarias e instat\u00e1neas), el analisis del riesgo de inundacion realizado para el municipio de navaluengo (avila) y la propuesta de su integracion con la plani<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Geomorfolog\u00eda e hidrolog\u00eda fluvial del rio alberche: modelos y s.i.g. para la gestion de riberas<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Geomorfolog\u00eda e hidrolog\u00eda fluvial del rio alberche: modelos y s.i.g. para la gestion de riberas <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Andres Diez Herrero <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 28\/11\/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>Javier Pedraza Gilsaz<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: guillermina Garz\u00f3n heydt <\/li>\n<li>Francisco Ayala carcedo (vocal)<\/li>\n<li>gerardo Benito ferrandez (vocal)<\/li>\n<li> Diaz de teran mira Jos\u00e9 ramon (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Andres Diez Herrero Mediante tecnicas de an\u00e1lisis hidrol\u00f3gico y geomorfol\u00f3gico, y el empleo de herramientas matematicas e [&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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