{"id":86707,"date":"2018-03-10T00:11:20","date_gmt":"2018-03-10T00:11:20","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/transformaciones-biogeoqua%c2%admicas-y-flujos-de-carbono-en-la-ria-de-vigo-estudio-de-la-variacion-de-corta-escala\/"},"modified":"2018-03-10T00:11:20","modified_gmt":"2018-03-10T00:11:20","slug":"transformaciones-biogeoqua%c2%admicas-y-flujos-de-carbono-en-la-ria-de-vigo-estudio-de-la-variacion-de-corta-escala","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/transformaciones-biogeoqua%c2%admicas-y-flujos-de-carbono-en-la-ria-de-vigo-estudio-de-la-variacion-de-corta-escala\/","title":{"rendered":"Transformaciones biogeoqu\u00edmicas y flujos de carbono en la ria de vigo. estudio de la variaci\u00f3n de corta escala."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Gago Pi\u00f1eiro Jes\u00fas Manuel <\/strong><\/h2>\n<p>El objetivo de este trabajo es estudiar la transferencia de di\u00f3xido de carbono entre la superficie de la r\u00eda y la atm\u00f3sfera con especial atenci\u00f3n a los procesos biogeoqu\u00edmicos que afectan a esta, as\u00ed como la cuantificaci\u00f3n de los flujos de las distintas formas de carbono entre la r\u00eda y la plataforma.  es de destacar, que el conocimiento del ciclo del carbono en un ecosistema como es la r\u00eda de vigo, presenta un alto inter\u00e9s local, dada la relevante actividad socioecon\u00f3mica de esta. En la r\u00eda convergen intereses pesqueros marisqueros, industriales y tur\u00edstico, siendo especialmente importante la regulaci\u00f3n y conrol de las actividades que pudieran afectar de manera irreversible al equilibrio del ecosistema.  la memoria se divide en tres parte. En la primera, de introducci\u00f3n, (cap\u00edtulos 1 a 3) se describen el \u00e1rea de estudio y las metodolog\u00edas de an\u00e1lisis. En la segunda parte (cap\u00edtulo 4) se estudian los cambios hidrogr\u00e1ficos y biogeoqu\u00edmicos de corta escala temporal para distintas situaciones. En la tercera parte se hace una descripci\u00f3n del equipo de pco2 asi como de la variabilidad de esta variable tanto en el aire como en el mar y se calculan los flujos de di\u00f3xido de carbono entre la r\u00eda y la atm\u00f3sfera. Los cap\u00edtulos 8 y 9 se dedican al estudio del intercambio entre la r\u00eda y la plataforma y a la cuantificaci\u00f3n de los cambios biogeoqu\u00edmcios con un m\u00e9todo inverso.  al final, en el apartado de conclusiones se recapitulan los logros obtendios en el entendimiento de la biogeoqu\u00edmica y la regulaci\u00f3n del contenido de di\u00f3xido de carbono atmosf\u00e9rico de la r\u00eda de vigo.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Transformaciones biogeoqu\u00edmicas y flujos de carbono en la ria de vigo. estudio de la variaci\u00f3n de corta escala.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Transformaciones biogeoqu\u00edmicas y flujos de carbono en la ria de vigo. estudio de la variaci\u00f3n de corta escala. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Gago Pi\u00f1eiro Jes\u00fas Manuel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Vigo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 29\/09\/2000<\/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>Fiz Fern\u00e1ndez P\u00e9rez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: gabriel Roson porto <\/li>\n<li>  (vocal)<\/li>\n<li>  (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 Gago Pi\u00f1eiro Jes\u00fas Manuel El objetivo de este trabajo es estudiar la transferencia de di\u00f3xido de carbono [&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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