{"id":43817,"date":"2018-07-19T01:55:46","date_gmt":"2018-07-19T01:55:46","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/determinacion-del-coeficiente-de-difusion-de-materia-en-la-capa-limite-superficial-y-su-relacion-con-los-parametros-meteorologicos\/"},"modified":"2018-07-19T01:55:46","modified_gmt":"2018-07-19T01:55:46","slug":"determinacion-del-coeficiente-de-difusion-de-materia-en-la-capa-limite-superficial-y-su-relacion-con-los-parametros-meteorologicos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/determinacion-del-coeficiente-de-difusion-de-materia-en-la-capa-limite-superficial-y-su-relacion-con-los-parametros-meteorologicos\/","title":{"rendered":"Determinacion del coeficiente de difusion de materia en la capa limite superficial y su relacion con los parametros meteorologicos."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Julio Gonzalez Suarez <\/strong><\/h2>\n<p>Se determina el coeficiente de difusion de materia en la capa atmosferica mas proxima a la superficie terrestre basandose en la ecuacion de difusion y utilizando el elemento rn86220. Se ha medido este elemento en cuatro alturas utilizando camaras de desintegracion y la espectroscopia para el analisis de los filtros obteniendo asi la variacion de la concentracion con la altura. Una vez conocida esta forma de variacion  hemos calculado el coeficiente de difusion por el metodo del flujo  en varios puntos segun la direccion vertical. Los valores obtenidos durante la campa\u00f1a mayo 1976 a abril de 1977  la hemos representado en funcion de los factores meteorologicos  velocidad del viento  gradiente de temperatura y precipitacion.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Determinacion del coeficiente de difusion de materia en la capa limite superficial y su relacion con los parametros meteorologicos.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Determinacion del coeficiente de difusion de materia en la capa limite superficial y su relacion con los parametros meteorologicos. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Julio Gonzalez Suarez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Valladolid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1977<\/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>Jos\u00e9 Lu\u00eds Casanova Roque<\/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 Garmendia Iraundegui (vocal)<\/li>\n<li>Jos\u00e9 Casanova Colas (vocal)<\/li>\n<li> Gutierrez Suarez Juan  Jos\u00e9 (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Julio Gonzalez Suarez Se determina el coeficiente de difusion de materia en la capa atmosferica mas proxima [&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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