{"id":5731,"date":"1995-01-01T00:00:00","date_gmt":"1995-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1995\/01\/01\/evaluacion-de-la-recarga-y-comportamiento-de-la-zona-no-saturada-en-el-acuifero-almonte-marismas-huelva\/"},"modified":"1995-01-01T00:00:00","modified_gmt":"1995-01-01T00:00:00","slug":"evaluacion-de-la-recarga-y-comportamiento-de-la-zona-no-saturada-en-el-acuifero-almonte-marismas-huelva","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evaluacion-de-la-recarga-y-comportamiento-de-la-zona-no-saturada-en-el-acuifero-almonte-marismas-huelva\/","title":{"rendered":"Evaluacion de la recarga y comportamiento de la zona no saturada en el acuifero almonte-marismas (huelva)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Manuel Olias Alvarez <\/strong><\/h2>\n<p>En esta investigacion se aborda el estudio experimental de la recarga, y el papel que juega al respecto la zona no saturada, en el acuifero almonte-marismas (huelva). Se trata de un acuifero detritico de 2400 km2 de superficie, sobre el que se asienta el parque nacional de do\u00f1ana. En los balances hidricos realizados en distintas investigaciones previas existian diferencias apreciables en la evaluacion de la recarga, por lo que en esta tesis se establecio como uno de los principales objetivos la obtencion de la informacion experimental necesaria para una evaluacion mas ajustada de dicho termino del balance.  para ello se instalo una serie de parcelas experimentales en distintas condiciones litologicas, edaficas y de vegetacion. En estas estaciones se controlaron en continuo las variables meteorologicas precipitacion y temperatura, y el nivel piezometrico y la conductividad y temperatura del agua mediante data-ioggers y, con una periodicidad aproximadamente mensual, se realizaron perfiles de humedad del suelo mediante testificacion neutronica. Tambien se construyeron una pareja de lisimetros para evaluar, de forma inequivoca, los terminos del balance. Asimismo, se han utilizado diferentes tecnicas (perfiles isotopicos, ensayos de permeabilidad, analisis granulometricos, etc), encaminadas al mejor conocimiento de las caracteristicas hidraulicas de la zona no saturada y su influencia sobre la recarga. Finalmente, se realizo una modelizacion matematica de alguna de las parcelas experimentales estudiadas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evaluacion de la recarga y comportamiento de la zona no saturada en el acuifero almonte-marismas (huelva).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evaluacion de la recarga y comportamiento de la zona no saturada en el acuifero almonte-marismas (huelva). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Manuel Olias Alvarez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/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>Javier Cruz San Juli\u00e1n<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Francisco Javier Martinez Gil <\/li>\n<li>Antonio Sastre Merlin (vocal)<\/li>\n<li>Francisco Garc\u00eda Novo (vocal)<\/li>\n<li>Arsenio Gonzalez Martinez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Manuel Olias Alvarez En esta investigacion se aborda el estudio experimental de la recarga, y el papel [&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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