{"id":417,"date":"2021-11-23T23:24:30","date_gmt":"2021-11-23T23:24:30","guid":{"rendered":"https:\/\/natureduca.com\/docencia\/?p=417"},"modified":"2021-12-01T14:50:43","modified_gmt":"2021-12-01T14:50:43","slug":"ecologia-general-el-suelo-formacion","status":"publish","type":"post","link":"https:\/\/natureduca.com\/aula\/ecologia-general-el-suelo-formacion\/","title":{"rendered":"ECOLOG\u00cdA GENERAL &#8211; EL SUELO: FORMACI\u00d3N"},"content":{"rendered":"\t\t\t\t<div class=\"wp-block-uagb-table-of-contents uagb-toc__align-left uagb-toc__columns-1  uagb-block-e9470fb4      \"\n\t\t\t\t\tdata-scroll= \"1\"\n\t\t\t\t\tdata-offset= \"30\"\n\t\t\t\t\tstyle=\"\"\n\t\t\t\t>\n\t\t\t\t<div class=\"uagb-toc__wrap\">\n\t\t\t\t\t\t<div class=\"uagb-toc__title\">\n\t\t\t\t\t\t\tTabla de contenidos\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<div class=\"uagb-toc__list-wrap \">\n\t\t\t\t\t\t<ol class=\"uagb-toc__list\"><li class=\"uagb-toc__list\"><a href=\"#los-factores-que-intervienen-en-la-formaci\u00f3n-del-suelo\" class=\"uagb-toc-link__trigger\">Los factores que intervienen en la formaci\u00f3n del suelo<\/a><ul class=\"uagb-toc__list\"><li class=\"uagb-toc__list\"><a href=\"#morrenas-glaciales\" class=\"uagb-toc-link__trigger\">Morrenas glaciales<\/a><li class=\"uagb-toc__list\"><li class=\"uagb-toc__list\"><a href=\"#meteorizaci\u00f3n\" class=\"uagb-toc-link__trigger\">Meteorizaci\u00f3n<\/a><\/ul><\/ol>\t\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\n\n\n<p class=\"has-drop-cap\">Aunque la ecolog\u00eda tambi\u00e9n se ocupa del estudio del suelo, es en realidad otra ciencia que se encuentra entre la biolog\u00eda y la&nbsp;geolog\u00eda, denominada&nbsp;<em>edafolog\u00eda<\/em>, la encargada de su estudio integral.<\/p>\n\n\n\n<p>Por su parte, la ecolog\u00eda considera al suelo y sus factores&nbsp;abi\u00f3ticos&nbsp;como actuantes sobre los seres vivos, y lo define dentro del ecosistema global como un ecosistema particular.<\/p>\n\n\n\n<p class=\"has-text-align-center\"><img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/images_cienc\/cienc_suelo2.jpg\" alt=\" \"><br><img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/images_cienc\/cienc_suelo.jpg\" alt=\" \">&nbsp;<img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/images_cienc\/ciencia_suelo3.jpg\" alt=\" \"><br>Los suelos son estructuras din\u00e1micas que van cambiando desde sus inicios hasta adquirir un equilibrio con el entorno<\/p>\n\n\n\n<p>A la capa superficial de la corteza terrestre donde se desarrollan las ra\u00edces de los vegetales se le denomina&nbsp;<em>suelo<\/em>. Duchafour lo defini\u00f3 como un medio complejo, cuyas caracter\u00edsticas son: atm\u00f3sfera interna, r\u00e9gimen h\u00eddrico particular, fauna y flora determinadas y elementos minerales. Se trata de estructuras din\u00e1micas que van cambiando desde sus inicios hasta adquirir un equilibrio con el entorno, aunque en el proceso de formaci\u00f3n pueden llegar a ser destruidos por la erosi\u00f3n.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Los factores que intervienen en la formaci\u00f3n del suelo<\/h2>\n\n\n\n<p>Al proceso de formaci\u00f3n y desarrollo de los suelos se le denomina&nbsp;<em>edafog\u00e9nesis<\/em>. Los factores que intervienen en este proceso son: el clima, el relieve, la actividad biol\u00f3gica, la composici\u00f3n litol\u00f3gica y el tiempo de actuaci\u00f3n de todos ellos.<\/p>\n\n\n\n<p>La materia org\u00e1nica es proporcionada por los&nbsp;animales&nbsp;y vegetales colonizadores del sustrato inorg\u00e1nico; El clima es el m\u00e1s importante de ellos, ya que determina el volumen de precipitaciones y la temperatura a la que tienen lugar las alteraciones qu\u00edmicas necesarias.<\/p>\n\n\n\n<p>El relieve facilita o dificulta, seg\u00fan el grado de inclinaci\u00f3n de la superficie, la infiltraci\u00f3n del agua en el terreno; cuanto mayor sea \u00e9sta, m\u00e1s activo ser\u00e1 el proceso edafogen\u00e9tico; el relieve tambi\u00e9n determina el grado de erosi\u00f3n y la orientaci\u00f3n con respecto al sol; las zonas dirigidas al sur sufren una mayor evaporaci\u00f3n y sus suelos son menos potentes.<\/p>\n\n\n\n<p>La actividad biol\u00f3gica favorece la disgregaci\u00f3n f\u00edsica de la roca madre (consistente en rocas sedimentarias y\/o morrenas glaciales), fundamentalmente mediante la acci\u00f3n de las ra\u00edces de los vegetales, pero tambi\u00e9n interviene de forma notable en la meteorizaci\u00f3n qu\u00edmica por medio de los \u00e1cidos h\u00famicos, procedentes de la descomposici\u00f3n de restos org\u00e1nicos. La composici\u00f3n litol\u00f3gica de la roca madre determina cu\u00e1les ser\u00e1n los productos de alteraci\u00f3n originados por la meteorizaci\u00f3n; por tanto, influye en el grado de acidez del suelo resultante.<\/p>\n\n\n\n<p class=\"has-text-align-center\"><img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/images_cienc\/cienc_formacsuelo.gif\" alt=\" \"><br>Proceso de formaci\u00f3n de los suelos:<br>1-Roca madre; 2-Acci\u00f3n mec\u00e1nica (cambios de temperatura, hielo, etc.); 3-Acci\u00f3n qu\u00edmica del agua y de sus sales minerales; 4-Acci\u00f3n de los seres vivos; 5-Acci\u00f3n conjunta de todos las materias org\u00e1nicas e inorg\u00e1nicas.<\/p>\n\n\n\n<div class=\"wp-block-uagb-inline-notice uagb-inline_notice__outer-wrap uagb-inline_notice__align-left uagb-block-a2b2f959\"><h4 class=\"uagb-notice-title\">Morrenas glaciales<\/h4><div class=\"uagb-notice-text\"><p>Sedimentos de arena, grava y piedras depositados o transportados por los glaciares.<\/p><\/div><\/div>\n\n\n\n<p>La roca madre constituye el aporte de elementos minerales cuando se produce su disgregaci\u00f3n y descomposici\u00f3n; finalmente, con el transcurso del tiempo y la acci\u00f3n conjunta del clima y vegetaci\u00f3n, se produce la mezcla de los elementos entre s\u00ed y con el aire y agua.<\/p>\n\n\n\n<div class=\"wp-block-uagb-inline-notice uagb-inline_notice__outer-wrap uagb-inline_notice__align-left uagb-block-6ea0512e\"><h4 class=\"uagb-notice-title\">Meteorizaci\u00f3n<\/h4><div class=\"uagb-notice-text\"><p>Proceso por el cual las rocas son alteradas mec\u00e1nica y qu\u00edmicamente por acci\u00f3n de diversos agentes, principalmente atmosf\u00e9ricos.<\/p><\/div><\/div>\n\n\n\n<p>B\u00e1sicamente, de todo lo dicho anteriormente, se puede pueden distinguir una serie fases en el proceso de formaci\u00f3n de los suelos, el cual dura una media de 500 a\u00f1os, dependiendo de las caracter\u00edsticas climatol\u00f3gicas del lugar:<\/p>\n\n\n\n<ul class=\"wp-block-list\"><li>Meteorizaci\u00f3n de la roca madre (acci\u00f3n mec\u00e1nica por hielo, temperatura, etc.).<\/li><li>Acci\u00f3n qu\u00edmica inorg\u00e1nica (agua, sales minerales).<\/li><li>Acci\u00f3n biol\u00f3gica (descomposici\u00f3n de materias por los seres vivos que colonizan el suelo, tales como bacterias, hongos o protozoos).<\/li><li>Acci\u00f3n conjunta de todos las materias org\u00e1nicas e inorg\u00e1nicas. <\/li><\/ul>\n\n\n\n<p class=\"has-text-align-center\"> <a href=\"https:\/\/natureduca.com\/aula\/indice-ecologia\/\"><img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/logos\/1ciencia2.jpg\" alt=\" \"><br><span style=\"font-size: medium;\">\u00cdndice Ecolog\u00eda<\/span><\/a> <\/p>\n","protected":false},"excerpt":{"rendered":"<p>Aunque la ecolog\u00eda tambi\u00e9n se ocupa del estudio del suelo, es en realidad otra ciencia que se encuentra entre la biolog\u00eda y la&nbsp;geolog\u00eda, denominada&nbsp;edafolog\u00eda, la encargada de su estudio integral. Por su parte, la ecolog\u00eda considera al suelo y sus factores&nbsp;abi\u00f3ticos&nbsp;como actuantes sobre los seres vivos, y lo define dentro&#8230;<\/p>\n<p class=\"continue-reading-button\"> <a class=\"continue-reading-link\" href=\"https:\/\/natureduca.com\/aula\/ecologia-general-el-suelo-formacion\/\">Seguir leyendo&#8230;<i class=\"crycon-right-dir\"><\/i><\/a><\/p>\n","protected":false},"author":3,"featured_media":-1,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_uag_custom_page_level_css":"","footnotes":""},"categories":[7],"tags":[4,76,5,73],"class_list":["post-417","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-ecologia","tag-ecologia","tag-formacion","tag-general","tag-suelo"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>ECOLOG\u00cdA GENERAL - EL SUELO: FORMACI\u00d3N - Aula de Naturaleza educativa<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/natureduca.com\/aula\/ecologia-general-el-suelo-formacion\/\" \/>\n<meta property=\"og:locale\" content=\"es_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"ECOLOG\u00cdA GENERAL - EL SUELO: FORMACI\u00d3N - Aula de Naturaleza educativa\" \/>\n<meta property=\"og:description\" content=\"Aunque la ecolog\u00eda tambi\u00e9n se ocupa del estudio del suelo, es en realidad otra ciencia que se encuentra entre la biolog\u00eda y la&nbsp;geolog\u00eda, denominada&nbsp;edafolog\u00eda, la encargada de su estudio integral. 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