{"id":6415,"date":"1995-01-01T00:00:00","date_gmt":"1995-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1995\/01\/01\/morfologia-mineralogia-y-genesis-de-los-suelos-desarrollados-sobre-distintas-superficies-morfologicas-relacionadas-con-la-vertiente-norte-de-los-montes-de-toledo\/"},"modified":"1995-01-01T00:00:00","modified_gmt":"1995-01-01T00:00:00","slug":"morfologia-mineralogia-y-genesis-de-los-suelos-desarrollados-sobre-distintas-superficies-morfologicas-relacionadas-con-la-vertiente-norte-de-los-montes-de-toledo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/morfologia-mineralogia-y-genesis-de-los-suelos-desarrollados-sobre-distintas-superficies-morfologicas-relacionadas-con-la-vertiente-norte-de-los-montes-de-toledo\/","title":{"rendered":"Morfolog\u00eda, mineralogia y genesis de los suelos desarrollados sobre distintas superficies morfologicas relacionadas con la vertiente norte de los montes de toledo."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Elena Pardo Garcia <\/strong><\/h2>\n<p>La tesis doctoral trata de los suelos desarrollados sobre la ra\u00f1a y el sistema de terrazas del sector talavera-malpica (toledo) en la zona comprendida entre los montes de toledo y el rio tajo. La metodolog\u00eda empleada parte de la delimitacion de las distintas superficies morfologicas y de la localizacion, descripcion y muestreo de los perfiles representativos de los suelos mas evolucionados de tales unidades. El analisis subsiguiente de las muestras completo la caracterizacion morfologica, fisica, quimica, fisico-quimica y mineralogica de los suelos.  el tratamiento estadistico de los datos permitio definir grupos estables, especialmente en lo que se refiere a sus propiedades mineralogicas, que justifica la relacion entre los suelos y las diferentes unidades morfologicas sobre las que evolucionan: ra\u00f1as occidentales, intermedias y orientales, superficie de transicion y terrazas.  los resultados permiten realizar importantes conclusiones respecto a la genesis y evolucion del paisaje de la ra\u00f1a, a la evolucion y cronolog\u00eda de los procesos edafogeneticos, a las propiedades del suelo, al origen y caracteristicas del carbonato calcico en determinadas superficies justificandose su ausencia en otras, y a la clasificacion de los suelos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Morfolog\u00eda, mineralogia y genesis de los suelos desarrollados sobre distintas superficies morfologicas relacionadas con la vertiente norte de los montes de toledo.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Morfolog\u00eda, mineralogia y genesis de los suelos desarrollados sobre distintas superficies morfologicas relacionadas con la vertiente norte de los montes de toledo. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Elena Pardo Garcia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1995<\/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>Rafaela Marfil Perez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Guillermina Garz\u00f3n Heydt <\/li>\n<li>Luisa Torcal Sainz (vocal)<\/li>\n<li> Roquero De Laburu Carlos (vocal)<\/li>\n<li>Mario Nieves Bernabe (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Elena Pardo Garcia La tesis doctoral trata de los suelos desarrollados sobre la ra\u00f1a y el sistema [&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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