{"id":34884,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/suelos-y-vegetacion-en-los-afloramientos-volcanicos-neogenos-de-la-zona-litoral-del-sureste-peninsular\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"suelos-y-vegetacion-en-los-afloramientos-volcanicos-neogenos-de-la-zona-litoral-del-sureste-peninsular","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/suelos-y-vegetacion-en-los-afloramientos-volcanicos-neogenos-de-la-zona-litoral-del-sureste-peninsular\/","title":{"rendered":"Suelos y vegetacion en los afloramientos volcanicos neogenos de la zona litoral del sureste peninsular."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Mar\u00eda  Josefa Delgado Iniesta <\/strong><\/h2>\n<p>En este trabajo se hace un estudio detallado de los suelos desarrollados a partir de materiales volc\u00e1nicos ne\u00f3genos de la banda litoral comprendida entre el mar menor (murcia) y cabo de gata (almer\u00eda) as\u00ed como de la vegetaci\u00f3n de tomillar que sobre estos suelos se instala.  dichos suelos se han clasificado seg\u00fan f.A.O. (1994) y s.S.S. (1996), tambi\u00e9n se ha estudiado la mineralog\u00eda de las fracciones de arena y arcilla as\u00ed como de la roca madre. Por otra parte, se ha calculado el \u00e1rea m\u00ednima que se ha de muestrear para que los tomillares term\u00f3filos muricano- almerienses para que estos sean justamente representados. Para el dise\u00f1o de muestreo se ha utilizado un sistema de informaci\u00f3n geogr\u00e1fica (gis). Se han realizado en diferentes puntos de muestreo toma de inventarios fitosociol\u00f3gicos y muestras de capa arable las cuales fueron analizadas en el laboratorio. Con los resultados obtenidos del an\u00e1lisis de las muestras de capa arable y de los inventarios fitosociol\u00f3gicos se ha efectuado diversas t\u00e9cnicas de ordenaci\u00f3n, en concreto un an\u00e1lisis indirecto de gradientes (an\u00e1lisis de correspondencia) y un an\u00e1lisis directo de gradientes (analisis de correspondencia can\u00f3nico). Con los grupos de muestras separados por este an\u00e1lisis directo se han comparado algunas de las variables ed\u00e1ficas medidas. Se presenta un esquema sintaxon\u00f3mico de las diferentes asociaciones vegetales que se han reconocido y un ap\u00e9ndice donde se recogen los resultados de los inventarios fitosociol\u00f3gicos para el c\u00e1lculo del \u00e1rea m\u00ednima as\u00ed como diversas tablas con los resultados anal\u00edticos obtenidos de las muestras de capa arable.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Suelos y vegetacion en los afloramientos volcanicos neogenos de la zona litoral del sureste peninsular.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Suelos y vegetacion en los afloramientos volcanicos neogenos de la zona litoral del sureste peninsular. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Mar\u00eda  Josefa Delgado Iniesta <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Murcia<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/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>Roque Ortiz Silla<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Mar\u00eda  Luisa Tejedor Salguero <\/li>\n<li>Mar\u00eda no Simon Torres (vocal)<\/li>\n<li>Joaquin Hernandez Bastida (vocal)<\/li>\n<li>Javier Loidi Arregui (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Mar\u00eda Josefa Delgado Iniesta En este trabajo se hace un estudio detallado de los suelos desarrollados a [&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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