{"id":137269,"date":"2026-01-12T17:04:12","date_gmt":"2026-01-12T17:04:12","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/adquisicion-de-los-contenidos-isotopicos-0-18-y-d-de-las-aguas-subterraneas-variaciones-en-la-atmosfera-y-en-la-zona-no-saturada-del-suelo\/"},"modified":"2026-01-12T17:04:12","modified_gmt":"2026-01-12T17:04:12","slug":"adquisicion-de-los-contenidos-isotopicos-0-18-y-d-de-las-aguas-subterraneas-variaciones-en-la-atmosfera-y-en-la-zona-no-saturada-del-suelo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/adquisicion-de-los-contenidos-isotopicos-0-18-y-d-de-las-aguas-subterraneas-variaciones-en-la-atmosfera-y-en-la-zona-no-saturada-del-suelo\/","title":{"rendered":"Adquisicion de los contenidos isotopicos 0-18 y d de las aguas subterraneas: variaciones en la atmosfera y en la zona no saturada del suelo"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Luis Araguas Araguas <\/strong><\/h2>\n<p>Establece un modelo isotopico de las precipitaciones en la peninsula iberica a escala anual y de precipitaciones angulares. Tambien obtiene perfiles de contenido isotopico en 0-18, d y tritio de la zona no saturada y analiza los mecanismos de recarga en la region de Madrid, en monion (huesca), delta del llobregat (barcelona), depresion de guadix-baza (granada) y do\u00f1ana (huelva).<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Adquisicion de los contenidos isotopicos 0-18 y d de las aguas subterraneas: variaciones en la atmosfera y en la zona no saturada del suelo<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Adquisicion de los contenidos isotopicos 0-18 y d de las aguas subterraneas: variaciones en la atmosfera y en la zona no saturada del suelo <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Luis Araguas Araguas <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Aut\u00f3noma de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1991<\/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>Fernando L\u00f3pez Vera<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Roberto Gonfiantini <\/li>\n<li>Jan Silar (vocal)<\/li>\n<li>Emilio Custodio Gimena (vocal)<\/li>\n<li>Javier Cruz San Juli\u00e1n (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Luis Araguas Araguas Establece un modelo isotopico de las precipitaciones en la peninsula iberica a escala anual [&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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