{"id":37108,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-edafologico-de-los-planosoles-del-campo-del-aranuelo\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"estudio-edafologico-de-los-planosoles-del-campo-del-aranuelo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-edafologico-de-los-planosoles-del-campo-del-aranuelo\/","title":{"rendered":"Estudio edafologico de los planosoles del campo del ara\u00f1uelo."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Jimenez Nasif Silvia Elena <\/strong><\/h2>\n<p>El presente trabajo de investigaci\u00f3n tiene por objetivo la caracterizaci\u00f3n edafol\u00f3gica de la comarca natural del campo ara\u00f1uelo, situada entre las provincias de c\u00e1ceres y toledo, con el fin de estudiar las condiciones de formaci\u00f3n de sus planosoles, as\u00ed como las principales causas de sus limitaciones agron\u00f3micas. Podemos afirmar que en esta comarca el rasgo natural que le imprime mayor car\u00e1cter es el suelo.  se comienza por hacer una exposici\u00f3n cr\u00edtico &#8211; anal\u00edtica del medio natural de dicha comarca haciendo especial \u00e9nfasis en los principales factores de formaci\u00f3n de sus suelos: clima, geomorfolog\u00eda, vegetaci\u00f3n y litolog\u00eda, sin olvidar los aspectos relacionados con la actividad humana.  del estudio, se deduce que los planosoles, siendo caracterizados por poseer horizontes arg\u00edlicos bt subsuperficiales y horizontes a y e por encima, separados por l\u00edmites generalmente abruptos, se asocian a superficies deprimidas y llanas.  los horizontes arg\u00edlicos se favorecen en su g\u00e9nesis por la alternancia estaci\u00f3n seca- estaci\u00f3n h\u00fameda, b\u00e1sica en el mecanismo de arranque de las part\u00edculas de arcilla dispersas de la matriz del suelo y su arrastre o iluviaci\u00f3n por el agua desde los horizontes a.  el desarrollo de los horizontes e y de muchas de las propiedades morfol\u00f3gicas caracter\u00edsticas relacionadas con la hidromorf\u00eda, se asocia a la presencia de dichos l\u00edmites abruptos, que propician la aparici\u00f3n de capas colgadas de agua as\u00ed como de lagunas superficiales que van a inducir la alternancia de ciclos de oxido-reducci\u00f3n, determinantes de la movilizaci\u00f3n, p\u00e9rdida y acumulaci\u00f3n a lo largo del perfil de los \u00f3xidos de fe.  son precisamente el encharcamiento temporal y la presencia del l\u00edmite abrupto los principales factores limitantes de su productividad.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio edafologico de los planosoles del campo del ara\u00f1uelo.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio edafologico de los planosoles del campo del ara\u00f1uelo. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Jimenez Nasif Silvia Elena <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Polit\u00e9cnica de Valencia<\/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>Juan  Manuel Gisbert Blanquer<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Bernardo Pascual Espa\u00f1a <\/li>\n<li>Elisa Barragan Landa (vocal)<\/li>\n<li>Rafael Espejo Serrano (vocal)<\/li>\n<li>Juan a P\u00e9rez Arias (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jimenez Nasif Silvia Elena El presente trabajo de investigaci\u00f3n tiene por objetivo la caracterizaci\u00f3n edafol\u00f3gica de la [&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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