{"id":33860,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evaluacion-del-carbono-de-suelos-de-zonas-semiaridas-en-la-perspectiva-de-los-fenomenos-de-cambio-climatico-global\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"evaluacion-del-carbono-de-suelos-de-zonas-semiaridas-en-la-perspectiva-de-los-fenomenos-de-cambio-climatico-global","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evaluacion-del-carbono-de-suelos-de-zonas-semiaridas-en-la-perspectiva-de-los-fenomenos-de-cambio-climatico-global\/","title":{"rendered":"Evaluacion del carbono de suelos de zonas semiaridas en la perspectiva de los fenomenos de cambio climatico global."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Diaz Hernandez Jos\u00e9 Luis <\/strong><\/h2>\n<p>Se considera al suelo como sumidero de di\u00f3xido de carb\u00f3nico: este hecho tiene enorme importancia en el balance del co2 atmosf\u00e9rico y en los fen\u00f3menos de retroalimentaci\u00f3n causados por cambios de vegetaci\u00f3n inducidos por el cambio clim\u00e1tico global.  es extremadamente importante para la modelizaci\u00f3n del cambio clim\u00e1tico, tener una evaluaci\u00f3n objetiva de formas de carbono almacenadas en los suelos de zonas semi\u00e1ridas.  por otro lado, en el caso del carbono inorg\u00e1nico los datos cartogr\u00e1ficos convencionales son inutilizables porque los perfiles taxon\u00f3micos no son suficientemente profundos.  en el trabajo desarrollado, se realiza una evaluaci\u00f3n del carbono org\u00e1nico e inorg\u00e1nico almacenado en los suelos del \u00e1rea de guadix-baza, de unos 6000 km2, hasta una profundidad de 4 m. Se analizan los problemas metodol\u00f3gicos de este tipo de inventario, y se efect\u00faa una evaluaci\u00f3n de la fracci\u00f3n de carbono de origen ed\u00e1fico presente en los suelos mediante la t\u00e9cnica de is\u00f3topos estables. Finalmente se estiman las tasas de secuestro de carbono en los suelos estudiados.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evaluacion del carbono de suelos de zonas semiaridas en la perspectiva de los fenomenos de cambio climatico global.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evaluacion del carbono de suelos de zonas semiaridas en la perspectiva de los fenomenos de cambio climatico global. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Diaz Hernandez Jos\u00e9 Luis <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/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>Enrique Barahona Fernandez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Antonio Vera Torres <\/li>\n<li> De La Rosa Acosta Diego (vocal)<\/li>\n<li>Jos\u00e9 Aguilar Ru\u00edz (vocal)<\/li>\n<li>Jos\u00e9 Luis Gonz\u00e1lez Rebollar (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Diaz Hernandez Jos\u00e9 Luis Se considera al suelo como sumidero de di\u00f3xido de carb\u00f3nico: este hecho tiene [&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":[20341,27,4329,2498,2752],"tags":[39614,91986,25750,2035,4294,35384],"class_list":["post-33860","post","type-post","status-publish","format-standard","hentry","category-cambio-climatico","category-ciencias-de-la-tierra-y-del-espacio","category-climatologia","category-edafologia","category-quimica-de-suelos","tag-de-la-rosa-acosta-diego","tag-diaz-hernandez-jose-luis","tag-enrique-barahona-fernandez","tag-jose-aguilar-ruiz","tag-jose-luis-gonzalez-rebollar","tag-juan-antonio-vera-torres"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/33860","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=33860"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/33860\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=33860"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=33860"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=33860"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}