{"id":49792,"date":"2021-05-16T07:51:02","date_gmt":"2021-05-16T07:51:02","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/hidrogeologia-del-terciario-en-el-borde-suroccidental-de-la-cuenca-del-duero\/"},"modified":"2021-05-16T07:51:02","modified_gmt":"2021-05-16T07:51:02","slug":"hidrogeologia-del-terciario-en-el-borde-suroccidental-de-la-cuenca-del-duero","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/hidrogeologia-del-terciario-en-el-borde-suroccidental-de-la-cuenca-del-duero\/","title":{"rendered":"Hidrogeolog\u00eda del terciario en el borde suroccidental de la cuenca del duero"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  S\u00e1nchez San Rom\u00e1n Francisco Javier <\/strong><\/h2>\n<p>Se estudia la hidrogeolog\u00eda del acuifero terciario atendiendo a todas las fases del ciclo hidrologico. Se calculan los valores medios de la plumometria y su variacion en a\u00f1os humedos y secos. Se estudia el fenomeno de la evapotranspiracion y se establecen balances de agua en el suelo. Se analizan los caudales de los rios tormes y guare\u00f1a y su evolucion en el tiempo. En el capitulo referente a hidrolog\u00eda subterranea se estudian especialmente las transmisividades  su distribucion espacial y su relacion con la geolog\u00eda. La evolucion de los niveles piezometricos permite delimitar las areas con un exceso de explotacion. Finalmente  se estudia el quimismo de las aguas subterraneas  la proporcion de los iones mayoritarios y silice y la relacion de todo ello con la geolog\u00eda y con el sistema de flujo subterraneo.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Hidrogeolog\u00eda del terciario en el borde suroccidental de la cuenca del duero<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Hidrogeolog\u00eda del terciario en el borde suroccidental de la cuenca del duero <\/li>\n<li><strong>Autor:<\/strong>\u00a0  S\u00e1nchez San Rom\u00e1n Francisco Javier <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1982<\/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>Francisco Javier Martinez Gil<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Antonio Arribas Moreno <\/li>\n<li>Carlos Garcia Figuerola (vocal)<\/li>\n<li>Manuel Ram\u00f3n Llamas Madruga (vocal)<\/li>\n<li>  (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de S\u00e1nchez San Rom\u00e1n Francisco Javier Se estudia la hidrogeolog\u00eda del acuifero terciario atendiendo a todas las fases [&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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