{"id":44646,"date":"2018-12-06T15:40:52","date_gmt":"2018-12-06T15:40:52","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/contribucion-al-estudio-de-la-difusion-de-materia-en-las-capas-bajas-de-la-atmosfera-cerca-de-la-discontinuidad-tierra-mar-utilizando-trazadores-radioactivos-naturales\/"},"modified":"2018-12-06T15:40:52","modified_gmt":"2018-12-06T15:40:52","slug":"contribucion-al-estudio-de-la-difusion-de-materia-en-las-capas-bajas-de-la-atmosfera-cerca-de-la-discontinuidad-tierra-mar-utilizando-trazadores-radioactivos-naturales","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/contribucion-al-estudio-de-la-difusion-de-materia-en-las-capas-bajas-de-la-atmosfera-cerca-de-la-discontinuidad-tierra-mar-utilizando-trazadores-radioactivos-naturales\/","title":{"rendered":"Contribucion al estudio de la difusion de materia en las capas bajas de la atmosfera cerca de la discontinuidad tierra-mar utilizando trazadores radioactivos naturales."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jes\u00fas Soto Torres <\/strong><\/h2>\n<p>Se utiliza el radon y la relacion entre las actividades del bi214 y del pb214 de terminados empiricamente mediante espectrometria gamma para caracterizar teorica y expirimentalmente las propiedades de difusion de las capas bajas de la atmosfera en un punto proximo a una discontinuidad importante en su superficie de exalacion.  para ello hemos resuelto numericamente la ecuacion de difusion y comparado los diferentes parametros meteorologicos con las concentraciones de radon encontradas a fin de conocer la importancia de cada uno de los posibles efectos que actuan sobre ellas. Partiendo de estos resultados se utiliza un modelo de caja cerrada para interpretar  comparando los resultados obtenidos mediante este con los experimentales  la variacion diaria de la estabilidad vertical. Por fin se estudia los factores que influyen sobre la relacion en el aire entre las actividades de los descendientes del radon.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Contribucion al estudio de la difusion de materia en las capas bajas de la atmosfera cerca de la discontinuidad tierra-mar utilizando trazadores radioactivos naturales.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Contribucion al estudio de la difusion de materia en las capas bajas de la atmosfera cerca de la discontinuidad tierra-mar utilizando trazadores radioactivos naturales. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jes\u00fas Soto Torres <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Cantabria<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1978<\/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>Eugenio Villar Garcia<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Catala De Alemany Joaquin <\/li>\n<li>Jos\u00e9 Aguilar Peris (vocal)<\/li>\n<li>Jos\u00e9 Garmendia Iraundegui (vocal)<\/li>\n<li>Leon Garzon Ruiperez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jes\u00fas Soto Torres Se utiliza el radon y la relacion entre las actividades del bi214 y del [&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":[10518,950,27,6118,429],"tags":[107867,103634,3515,7731,9685,108355],"class_list":["post-44646","post","type-post","status-publish","format-standard","hentry","category-cantabria","category-ciencias-de-la-atmosfera","category-ciencias-de-la-tierra-y-del-espacio","category-difusion-atmosferica","category-meteorologia","tag-catala-de-alemany-joaquin","tag-eugenio-villar-garcia","tag-jesus-soto-torres","tag-jose-aguilar-peris","tag-jose-garmendia-iraundegui","tag-leon-garzon-ruiperez"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/44646","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=44646"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/44646\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=44646"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=44646"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=44646"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}