{"id":142569,"date":"1993-01-01T00:00:00","date_gmt":"1993-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-quimico-y-mineralogico-de-suelos-desarrollados-sobre-gneis-y-migmatitas-variacion-en-la-composicion-de-minerales-de-arcilla-en-los-procesos-de-alteracion\/"},"modified":"1993-01-01T00:00:00","modified_gmt":"1993-01-01T00:00:00","slug":"estudio-quimico-y-mineralogico-de-suelos-desarrollados-sobre-gneis-y-migmatitas-variacion-en-la-composicion-de-minerales-de-arcilla-en-los-procesos-de-alteracion","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-quimico-y-mineralogico-de-suelos-desarrollados-sobre-gneis-y-migmatitas-variacion-en-la-composicion-de-minerales-de-arcilla-en-los-procesos-de-alteracion\/","title":{"rendered":"Estudio quimico y mineralogico de suelos desarrollados sobre gneis y migmatitas. variacion en la composicion de minerales de arcilla en los procesos de alteracion."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Barba Carretero Ana M. <\/strong><\/h2>\n<p>Se ha realizado un estudio quimico y mineralogico de suelos situados en tres catenas de un mismo valle, el valle de el paular, Madrid. Se trata de suelos caracteristicos de monta\u00f1a, sobre todo leptosoles y cambisoles, aunque en algun caso llegan a describirse phaeozems y luvisoles. Se constata la influencia de la posicion fisiografica y del tipo de vegetacion en el desarrollo de dichos suelos, puesto que se parte de una material original analogo en todos los casos. En cuanto al estudio mineralogico, se han empleado tecnicas de microscopia optica, difraccion de rayos x, estudio en lamina delgada y microscopia electronica de transmision; se ha llegado a establecer con dichas tecnicas la composicion mineral de las distintas fracciones granulometricas de los suelos, encontrando como mas caracteristica de cada suelo en concreto la fraccion arcilla. Los minerales de la fraccion arcilla presentan una serie de desviaciones respecto a los encontrados en las otras fracciones y en el material de partida, lo que ha hecho que merezcan una atencion especial y constituyan un capitulo importante.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio quimico y mineralogico de suelos desarrollados sobre gneis y migmatitas. variacion en la composicion de minerales de arcilla en los procesos de alteracion.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio quimico y mineralogico de suelos desarrollados sobre gneis y migmatitas. variacion en la composicion de minerales de arcilla en los procesos de alteracion. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Barba Carretero Ana M. <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1993<\/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: Juan a Gonzalez Parra <\/li>\n<li> Gandullo Gutierrez Jos\u00e9 Manuel (vocal)<\/li>\n<li>Mar\u00eda  Luisa Palomar Garcia Villamil (vocal)<\/li>\n<li> Hoyos Guerrero Miguel Angel (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Barba Carretero Ana M. Se ha realizado un estudio quimico y mineralogico de suelos situados en tres [&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":[27,986,2498,3977],"tags":[257255,16512,14708,5197,9822,92394],"class_list":["post-142569","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-complutense-de-madrid","category-edafologia","category-mineralogia-de-suelos","tag-barba-carretero-ana-m","tag-gandullo-gutierrez-jose-manuel","tag-hoyos-guerrero-miguel-angel","tag-juan-a-gonzalez-parra","tag-juan-hernando-costa","tag-maria-luisa-palomar-garcia-villamil"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/142569","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=142569"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/142569\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=142569"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=142569"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=142569"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}