{"id":33472,"date":"1997-11-12T00:00:00","date_gmt":"1997-11-12T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/marco-conceptual-y-desarrollo-metodologico-para-la-caracterizacion-y-modelado-de-caudales-de-compensacion-en-rios-mediterraneos-continentales-rio-lozoya-cuenca-rio-tajo-espana\/"},"modified":"1997-11-12T00:00:00","modified_gmt":"1997-11-12T00:00:00","slug":"marco-conceptual-y-desarrollo-metodologico-para-la-caracterizacion-y-modelado-de-caudales-de-compensacion-en-rios-mediterraneos-continentales-rio-lozoya-cuenca-rio-tajo-espana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/marco-conceptual-y-desarrollo-metodologico-para-la-caracterizacion-y-modelado-de-caudales-de-compensacion-en-rios-mediterraneos-continentales-rio-lozoya-cuenca-rio-tajo-espana\/","title":{"rendered":"Marco conceptual y desarrollo metodologico para la caracterizacion y modelado de caudales de compensacion en rios mediterraneos continentales (rio lozoya, cuenca rio tajo), espa\u00f1a."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Alberto Martin Zazo <\/strong><\/h2>\n<p>Con el objeto de caracterizar la variaci\u00f3n espacial y temporal de la hidroqu\u00edmica del agua y la estructura y composici\u00f3n de la comunidad de macroinvertebrados, en el eje principal del r\u00edo lozoya, en relaci\u00f3n con el r\u00e9gimen h\u00eddrico anual y en funci\u00f3n de la regulaci\u00f3n, se seleccionaron tres estaciones de muestreo: un primer tramo natural no regulado (alameda del valle), un tramo medio debajo de un embalse aislado (pinilla) y un tramo final tras la cadena de embalses (aguas abajo del pont\u00f3n de la oliva).  en el primer arroyo del tramo alto, el r\u00e9gimen h\u00eddrico presenta cierta variabilidad estacional, respondiendo su hidroqu\u00edmica en primer lugar a las litofacies drenadas y al balance precipitaci\u00f3n-evaporaci\u00f3n. Las comunidades bent\u00f3nicas presentan un elevado valor ambiental. Aguas abajo de pinilla, se origina una homogeneizaci\u00f3n de las temperaturas del agua, produciendo una mayor constancia t\u00e9rmica a lo largo del a\u00f1o. Se observa as\u00edmismo, una reducci\u00f3n dr\u00e1stica de los valores de diversidad, a\u00fan cuando los valores de densidad se mantienen constantes.  la estaci\u00f3n tres, es la m\u00e1s equilibrada, organizada y diversa.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Marco conceptual y desarrollo metodologico para la caracterizacion y modelado de caudales de compensacion en rios mediterraneos continentales (rio lozoya, cuenca rio tajo), espa\u00f1a.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Marco conceptual y desarrollo metodologico para la caracterizacion y modelado de caudales de compensacion en rios mediterraneos continentales (rio lozoya, cuenca rio tajo), espa\u00f1a. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Alberto Martin Zazo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Aut\u00f3noma de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 11\/12\/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>Carmen Casado Sancho<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carlos Montes del olmo <\/li>\n<li>diego Garcia de jalon (vocal)<\/li>\n<li>rosario Vidal abarca (vocal)<\/li>\n<li>Mar\u00eda Luisa Su\u00e1rez alonso (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alberto Martin Zazo Con el objeto de caracterizar la variaci\u00f3n espacial y temporal de la hidroqu\u00edmica del [&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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