{"id":12049,"date":"2001-06-07T00:00:00","date_gmt":"2001-06-07T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-hidrogeoquimica-del-macizo-de-betancuria-fuerteventura-archipielago-de-canarias\/"},"modified":"2001-06-07T00:00:00","modified_gmt":"2001-06-07T00:00:00","slug":"caracterizacion-hidrogeoquimica-del-macizo-de-betancuria-fuerteventura-archipielago-de-canarias","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/caracterizacion-hidrogeoquimica-del-macizo-de-betancuria-fuerteventura-archipielago-de-canarias\/","title":{"rendered":"Caracterizacion hidrogeoquimica del macizo de betancuria, fuerteventura, archipielago de canarias"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Christian Herrera Lameli <\/strong><\/h2>\n<p>La isla de fuerteventura se situa en el borde oriental del archipielago de canarias,a solo 100 km del continente africano. Presente un relieve topografico relativamente suave respecto a las otras islas de archipielago, lo que unido a su proximidad a la costa del sahara explican el car\u00e1cter arido del clima imperante.  el sector estudiado se situa en la parte central de la isla y abarca gran parte del macizo de betancuria y de la depresion central. A partir de la distribuci\u00f3n de las unidades geologicas e hidrogeol\u00f3gicas mas importantes se ha dividido el area de estudio en dos dominios principales: un dominio occidental, constituido por rocas volcanicas e intrusivas del complejo basal (cretacico superior-mioceno inferior) y un dominio oriental, compuesto por lavas del edificio gran tarajal (mioceno) y por depositos volcanicos (pleistoceno-holoceno) que conforman el malpais.  se ha realizado una estimacion de la recarga por medio de un balance hidrometeorol\u00f3gico de precipitacion diario y por medio de un balance de cloruros. Los calculos obtenidos a partir del balance hidrometerol\u00f3gico indican que la recarga varia significativamente seg\u00fan la situacion espacial de cada punto, obteniendose valores entre un 5y 20% de la precipitacion en las partes mas altas, mientras que en las zonas mas bajas esta es casi nula. Por otro lado, el calculo obtenido a partir del balance de cloruros indca que en ciertas zonas m\u00e1s bajas,donde posiblemente se registran importantes encharcamientos de aguas de tormenta, la recarga puede ser mayor, alcazado entre un 9 y 19% de la precipitacion.  en el dominio occidental las aguas subterraneas se caracterizan por presentar un aumentode la salinidad con la profundidad. Asi se puede diferenciar una unidad superior, que contiene aguas de menor conductividad electrica (2.5-5.5 ms\/cm) y temperaturas que varian entre los 18 y los 25\u00c2\u00ba c, y una unidad inferior,con aguas de mayor conductividad electrica (5.5-24 ms\/cm) y<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracterizacion hidrogeoquimica del macizo de betancuria, fuerteventura, archipielago de canarias<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracterizacion hidrogeoquimica del macizo de betancuria, fuerteventura, archipielago de canarias <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Christian Herrera Lameli <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Polit\u00e9cnica de catalunya<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 06\/07\/2001<\/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>Emilio Custodio Gimena<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jes\u00fas Carrera ram\u00edrez <\/li>\n<li>marisol Manzano arellano (vocal)<\/li>\n<li>Andr\u00e9s Sahuquillo herr\u00e1iz (vocal)<\/li>\n<li> Cabrera santana M\u00aa carmen (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Christian Herrera Lameli La isla de fuerteventura se situa en el borde oriental del archipielago de canarias,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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