{"id":31884,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-multifractal-de-la-distribucion-de-la-porosidad-del-suelo\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"analisis-multifractal-de-la-distribucion-de-la-porosidad-del-suelo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/analisis-multifractal-de-la-distribucion-de-la-porosidad-del-suelo\/","title":{"rendered":"Analisis multifractal de la distribucion de la porosidad del suelo."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Caniego Monreal Francisco Javier <\/strong><\/h2>\n<p>El objetivo de este trabajo es aplicar el analisis multifractal al estudio de la distribucion de la porosidad (area-tama\u00f1o de poro), evaluando el grado de definicion de las dimensiones multifractales o espectro multifractal, que permitan la caracterizacion de su complejidad. Los datos utilizados fueron obtenidos mediante analisis de imagen de muestras de suelo.  despues de exponer los elementos basicos de edafolog\u00eda relativos a la estructura, se presenta una seleccion de los ultimos trabajos que aplican la geometria fractal al estudio de la porosidad del suelo.  se introducen los conceptos fundamentales de la teoria de la medida, teoria de la informacion y geometria fractal, los cuales aparecen relacionados posteriormente en el desarrollo del analisis multifractal.  el problema de la evaluacion del espectro es considerado y resuelto con la seleccion de un metodo adecuado para nuestro objetivo concreto, que evita ciertas dificultades tecnicas que otros metodos plantean.  finalmente, los resultados obtenidos son analizados mostrando unas dimensiones multifractales bien definidas, de manera especial en el caso de la dimension de entropia.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Analisis multifractal de la distribucion de la porosidad del suelo.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Analisis multifractal de la distribucion de la porosidad del suelo. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Caniego Monreal Francisco Javier <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Polit\u00e9cnica de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/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> Martin Martin Miguel Angel<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Taguas Coejo Fco. Javier <\/li>\n<li> De Guzman Ozamiz Miguel (vocal)<\/li>\n<li>Francisco Javier Elorza Tenreiro (vocal)<\/li>\n<li>Juan  Vicente Giraldez Cervera (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Caniego Monreal Francisco Javier El objetivo de este trabajo es aplicar el analisis multifractal al estudio de [&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":[3183,27,2498,2497,126,3385,16008],"tags":[88496,4255,30392,1986,24223,88497],"class_list":["post-31884","post","type-post","status-publish","format-standard","hentry","category-analisis-y-analisis-funcional","category-ciencias-de-la-tierra-y-del-espacio","category-edafologia","category-fisica-de-suelos","category-matematicas","category-medida-integracion-y-area","category-politecnica-de-madrid","tag-caniego-monreal-francisco-javier","tag-de-guzman-ozamiz-miguel","tag-francisco-javier-elorza-tenreiro","tag-juan-vicente-giraldez-cervera","tag-martin-martin-miguel-angel","tag-taguas-coejo-fco-javier"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/31884","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=31884"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/31884\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=31884"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=31884"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=31884"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}