{"id":128425,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/degradacion-de-suelos-por-erosion-hidrica-en-la-cuenca-del-duero-estabilidad-estructural-y-estimacion-de-la-escorrentia-superficial\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"degradacion-de-suelos-por-erosion-hidrica-en-la-cuenca-del-duero-estabilidad-estructural-y-estimacion-de-la-escorrentia-superficial","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/degradacion-de-suelos-por-erosion-hidrica-en-la-cuenca-del-duero-estabilidad-estructural-y-estimacion-de-la-escorrentia-superficial\/","title":{"rendered":"Degradacion de suelos por erosion hidrica en la cuenca del duero. estabilidad estructural y estimacion de la escorrentia superficial."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Casermeiro Martinez Miguel Angel <\/strong><\/h2>\n<p>Se estudian los procesos de erosion hidrica en tres cuencas tributarias del duero. En los paramos aparecen luvisoles y leptosoles bajo vegetacion forestal con alta estabilidad estructural y baja erodibilidad. En las cuestas y laderas se situan cambisoles, regosoles, leptosoles y arenosoles. Los regosoles presentan bajos valores de cobertura vegetal y estabilidad estructural, altos valores de escorrentia y perdida de sedimentos, con suelos facilmente erosionables. Los cambisoles con alta cobertura., Estabilidad estructural e infiltracion, con sueros dificilmente erosionables a pesar de situarse en pendientes. Los arenosoles sin agregados estructurales y con altos valores de escorrentia y perdida de sedimentos son asimismo facilmente erosionables. En el rio duero se localizan fluvisoles cultivados con alta estabilidad estructural, baja escorrentia y perdida de sedimentos por lo que son muy poco erosionables.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Degradacion de suelos por erosion hidrica en la cuenca del duero. estabilidad estructural y estimacion de la escorrentia superficial.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Degradacion de suelos por erosion hidrica en la cuenca del duero. estabilidad estructural y estimacion de la escorrentia superficial. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Casermeiro Martinez Miguel Angel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Juan Hernando Costa<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Concepcion Gonzalez Huecas <\/li>\n<li>Jos\u00e9 Forteza Bonin (vocal)<\/li>\n<li>Roque Ortiz Silla (vocal)<\/li>\n<li>Jos\u00e9 Antonio Egido Rodriguez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Casermeiro Martinez Miguel Angel Se estudian los procesos de erosion hidrica en tres cuencas tributarias del duero. [&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":[16509,27,986,3238,2498,1666],"tags":[42084,187537,109300,240457,9822,22050],"class_list":["post-128425","post","type-post","status-publish","format-standard","hentry","category-aguas-superficiales","category-ciencias-de-la-tierra-y-del-espacio","category-complutense-de-madrid","category-conservacion-de-suelos","category-edafologia","category-hidrologia","tag-casermeiro-Martinez-miguel-angel","tag-concepcion-gonzalez-huecas","tag-jose-antonio-egido-rodriguez","tag-jose-forteza-bonin","tag-juan-hernando-costa","tag-roque-ortiz-silla"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/128425","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=128425"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/128425\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=128425"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=128425"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=128425"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}