{"id":122023,"date":"2024-06-24T09:08:17","date_gmt":"2024-06-24T09:08:17","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/hidrogeologia-regional-de-la-depresion-del-campo-aranuelo\/"},"modified":"2024-06-24T09:08:17","modified_gmt":"2024-06-24T09:08:17","slug":"hidrogeologia-regional-de-la-depresion-del-campo-aranuelo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/hidrogeologia-regional-de-la-depresion-del-campo-aranuelo\/","title":{"rendered":"Hidrogeolog\u00eda regional de la depresion del campo ara\u00f1uelo."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Rosa Vicente Lapuente <\/strong><\/h2>\n<p>Se estudia la estructura hidrogeologica de la depresion del campo ara\u00f1uelo. Para ello se analizan las caracteristicas climaticas de la region y se obtienen parametros hidraulicos del sustrato. Se elabora la red de flujo y se relacionan las caracteristicas fisico-quimicas de las aguas subterraneas con la distribucion del potencial obtenido. A los datos fisico-quimicos de las aguas subterraneas se les aplica el wategf y se efectua un tratamiento estadistico tanto de los datos fisico-quimicos como de los datos de saturacion del agua estudiando la distribucion espacial de los diversos factores mediante el analisis de las superficies de tendencia.  el estudio del agua clorurado-sodico-calcica muy mineralizada  existente en los bordes de la depresion procedente de los granitos lleva a proponer un modeloglobal del funcionamiento hidraulico e hidroquimico de la depresion del campo ara\u00f1uelo  segun el cual existiria un flujo de agua  muy lento  procedente de losgranitos que descargaria en la depresion debido a su menor potencial hidraulico.Alli las aguas procedentes de los granitos se mezclarian con las de la fosa dando lugar a la precipitacion de co sub 3 ca y a una granja de agua clorurado-sodica sobre aquella.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Hidrogeolog\u00eda regional de la depresion del campo ara\u00f1uelo.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Hidrogeolog\u00eda regional de la depresion del campo ara\u00f1uelo. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Rosa Vicente Lapuente <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Alcal\u00e1<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1986<\/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>Antonio Sastre Merlin<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Javier Cruz San Juli\u00e1n <\/li>\n<li> Lopez-camacho Y Camacho  Bernardo (vocal)<\/li>\n<li>Javier Martinez Gil (vocal)<\/li>\n<li>Ferm\u00edn Villarroya Gil (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Rosa Vicente Lapuente Se estudia la estructura hidrogeologica de la depresion del campo ara\u00f1uelo. Para ello se [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[3498,17426,27,953,3499,1666],"tags":[22215,17430,3778,111798,89221,88640],"class_list":["post-122023","post","type-post","status-publish","format-standard","hentry","category-aguas-subterraneas","category-alcala","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-hidrogeologia","category-hidrologia","tag-antonio-sastre-merlin","tag-fermin-villarroya-gil","tag-javier-cruz-san-julian","tag-javier-Martinez-gil","tag-lopez-camacho-y-camacho-bernardo","tag-rosa-vicente-lapuente"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/122023","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=122023"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/122023\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=122023"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=122023"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=122023"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}