{"id":427,"date":"2021-11-24T08:42:50","date_gmt":"2021-11-24T08:42:50","guid":{"rendered":"https:\/\/natureduca.com\/docencia\/?p=427"},"modified":"2021-12-01T15:00:56","modified_gmt":"2021-12-01T15:00:56","slug":"ecologia-general-el-suelo-erosion-1a-parte","status":"publish","type":"post","link":"https:\/\/natureduca.com\/aula\/ecologia-general-el-suelo-erosion-1a-parte\/","title":{"rendered":"ECOLOG\u00cdA GENERAL &#8211; EL SUELO: EROSI\u00d3N &#8211; 1\u00aa PARTE"},"content":{"rendered":"\t\t\t\t<div class=\"wp-block-uagb-table-of-contents uagb-toc__align-left uagb-toc__columns-1  uagb-block-fee144c0      \"\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-agentes-causantes-de-la-erosi\u00f3n\" class=\"uagb-toc-link__trigger\">Los agentes causantes de la erosi\u00f3n<\/a><ul class=\"uagb-toc__list\"><li class=\"uagb-toc__list\"><a href=\"#erosi\u00f3n-e\u00f3lica\" class=\"uagb-toc-link__trigger\">Erosi\u00f3n e\u00f3lica<\/a><li class=\"uagb-toc__list\"><li class=\"uagb-toc__list\"><a href=\"#erosi\u00f3n-fluvial\" class=\"uagb-toc-link__trigger\">Erosi\u00f3n fluvial<\/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\">La erosi\u00f3n de los suelos es un proceso natural producto de la acci\u00f3n de los agentes atmosf\u00e9ricos, aunque esta acci\u00f3n se ve fortalecida por las actividades humanas.<\/p>\n\n\n\n<p>Espa\u00f1a es un ejemplo de ese proceso des\u00e9rtico, con una cuarta parte de la superficie bajo sus efectos, que provoca anualmente un mill\u00f3n de toneladas de p\u00e9rdida de suelo vegetal, causado mayormente por las caracter\u00edsticas f\u00edsicas de gran parte del territorio, de marcada orograf\u00eda y grandes extensiones de suelos arcillosos, los cuales son f\u00e1cilmente erosionables por la acci\u00f3n de las lluvias, apoyados por el clima mediterr\u00e1neo cuyos aguaceros se concentran fuertemente y en poco tiempo.<\/p>\n\n\n\n<p class=\"has-text-align-center\"><img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/images_cienc\/cienc_desertizacion.jpg\" alt=\" \"><br>La erosi\u00f3n continuada de los suelos<br>culmina con la desertizaci\u00f3n<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Los agentes causantes de la erosi\u00f3n<\/h2>\n\n\n\n<p>Durante el proceso de erosi\u00f3n se arranca y transporta las capas superficiales de la tierra vegetal. Los agentes externos causantes de la erosi\u00f3n y modelaci\u00f3n de la corteza terrestre son esencialmente: la&nbsp; intemperie; el viento (erosi\u00f3n e\u00f3lica); las aguas superficiales (erosiones pluvial y fluvial); las aguas subterr\u00e1neas; los glaciares; el mar y los organismos lit\u00f3fagos.<\/p>\n\n\n\n<p class=\"has-text-align-center\"><img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/images_cienc\/cienc_erosion1.jpg\" alt=\" \"><br>El proceso f\u00edsico y qu\u00edmico de la erosi\u00f3n destruye continuamente suelos y rocas de la superficie terrestre<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">Erosi\u00f3n e\u00f3lica<\/h3>\n\n\n\n<p>La erosi\u00f3n e\u00f3lica es llevada a cabo por el viento y es cuantitativamente menos importante que las dem\u00e1s; est\u00e1 condicionada a la ausencia de vegetaci\u00f3n y a la presencia de part\u00edculas sueltas en la superficie.<\/p>\n\n\n\n<p>La deflaci\u00f3n se produce cuando el viento levanta los fragmentos sueltos del suelo; la abrasi\u00f3n tiene lugar cuando dichos fragmentos chocan con la superficie de las rocas y las desgastan; en las rocas de consistencia heterog\u00e9nea la erosi\u00f3n avanza m\u00e1s r\u00e1pidamente en las zonas m\u00e1s blandas, produciendo una superficie denominada alveolar.<\/p>\n\n\n\n<h3 class=\"wp-block-heading\">Erosi\u00f3n fluvial<\/h3>\n\n\n\n<p>La erosi\u00f3n fluvial es la que llevan a cabo los cursos de agua continentales (r\u00edos y torrentes); la energ\u00eda cin\u00e9tica del agua determina la intensidad de la erosi\u00f3n y depende de la energ\u00eda potencial, que se debe a la diferencia de altura entre la zona donde discurre y el nivel del mar (nivel de base).<\/p>\n\n\n\n<p class=\"has-text-align-center\"><img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/images_cienc\/cienc_erosion3.jpg\" alt=\" \">&nbsp;<img title=\" \"decoding=\"async\" src=\"https:\/\/natureduca.com\/images_cienc\/cienc_erosion2.jpg\" alt=\" \"><br>Las aguas fluviales y subterr\u00e1neas son agentes externos causantes de la erosi\u00f3n<\/p>\n\n\n\n<p>La energ\u00eda cin\u00e9tica no es uniforme a lo largo del curso del r\u00edo y es mayor en el tramo alto, de mayor pendiente, y menor en la desembocadura; ello determina una erosi\u00f3n diferencial que modifica el perfil longitudinal del curso del r\u00edo, evolucionando hacia un modelo te\u00f3rico, el denominado perfil de equilibrio, en el que cada punto del mismo recibe por sedimentaci\u00f3n la misma cantidad de materiales que pierde por erosi\u00f3n. Los cambios de nivel de base (transgresiones y regresiones marinas) determinan un nuevo perfil de equilibrio.<\/p>\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>La erosi\u00f3n de los suelos es un proceso natural producto de la acci\u00f3n de los agentes atmosf\u00e9ricos, aunque esta acci\u00f3n se ve fortalecida por las actividades humanas. Espa\u00f1a es un ejemplo de ese proceso des\u00e9rtico, con una cuarta parte de la superficie bajo sus efectos, que provoca anualmente un mill\u00f3n&#8230;<\/p>\n<p class=\"continue-reading-button\"> <a class=\"continue-reading-link\" href=\"https:\/\/natureduca.com\/aula\/ecologia-general-el-suelo-erosion-1a-parte\/\">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":[4,82,5,38,73],"class_list":["post-427","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-ecologia","tag-ecologia","tag-erosion","tag-general","tag-parte","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: EROSI\u00d3N - 1\u00aa PARTE - 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-erosion-1a-parte\/\" \/>\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: EROSI\u00d3N - 1\u00aa PARTE - Aula de Naturaleza educativa\" \/>\n<meta property=\"og:description\" content=\"La erosi\u00f3n de los suelos es un proceso natural producto de la acci\u00f3n de los agentes atmosf\u00e9ricos, aunque esta acci\u00f3n se ve fortalecida por las actividades humanas. 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Espa\u00f1a es un ejemplo de ese proceso des\u00e9rtico, con una cuarta parte de la superficie bajo sus efectos, que provoca anualmente un mill\u00f3n... 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