{"id":421,"date":"2021-11-23T23:33:02","date_gmt":"2021-11-23T23:33:02","guid":{"rendered":"https:\/\/natureduca.com\/docencia\/?p=421"},"modified":"2021-12-01T14:52:22","modified_gmt":"2021-12-01T14:52:22","slug":"ecologia-general-el-suelo-composicion-quimica-1a-parte","status":"publish","type":"post","link":"https:\/\/natureduca.com\/aula\/ecologia-general-el-suelo-composicion-quimica-1a-parte\/","title":{"rendered":"ECOLOG\u00cdA GENERAL – EL SUELO: COMPOSICI\u00d3N QU\u00cdMICA – 1\u00aa PARTE"},"content":{"rendered":"\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t
\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
\n\t\t\t\t\t\t
  1. Arena<\/a>
  2. Arcillas<\/a>
  3. Caliza<\/a>
  4. \u00d3xidos de hierro<\/a><\/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

    e puede dividir la composici\u00f3n qu\u00edmica de los suelos en org\u00e1nicos e inorg\u00e1nicos. Representan las part\u00edculas minerales el 50% del total, de las cuales dominan la arena, arcilla y caliza, y en menor medida \u00f3xidos e hidr\u00f3xidos de hierro y sales; las de origen org\u00e1nico suponen el 5%; el 45% que resta lo ocupan aire y agua, los cuales aprovechan la porosidad de la arena (el componente m\u00e1s importante de los suelos) para penetrar en los suelos y permitir la iteraci\u00f3n con los dem\u00e1s elementos.<\/p>\n\n\n\n

    Arena<\/h2>\n\n\n\n

    La arena, cuya importancia ya se ha dicho, procede de la roca por meteorizaci\u00f3n<\/em> (efectos externos que alteran las rocas superficiales); la sil\u00edcica es la m\u00e1s t\u00edpica, por ello se suele expresar el contenido de arena de los suelos en tanto por ciento de s\u00edlice (SiO2).<\/p>\n\n\n\n

    \"
    La arena procede de la meteorizaci\u00f3n de la roca madre<\/p>\n\n\n\n

    Arcillas<\/h2>\n\n\n\n

    Las arcillas proceden de silicatos descompuestos de la roca madre. Son principalmente una mezcla de silicatos de aluminio hidratados, los cuales pueden incorporar adem\u00e1s hierro, magnesio y potasio. La m\u00e1s t\u00edpica es la caolinita (s\u00edlice, al\u00famina y agua).<\/p>\n\n\n\n

    \"
    Las arcillas proceden de silicatos descompuestos de la roca madre<\/p>\n\n\n\n

    La presencia dominante de los silicatos de aluminio es la raz\u00f3n de que el contenido en arcilla de los suelos, sea expresada en tantos por ciento de \u00f3xido alum\u00ednico o al\u00famina (A12O3).<\/p>\n\n\n\n

    Caliza<\/h2>\n\n\n\n

    La caliza o carbonato c\u00e1lcico (CaCO3), suele presentarse en forma de arenas, limos o unidas a las arcillas margosas. Tienen la capacidad de disolverse en el agua, las cuales arrastran en forma de bicarbonato c\u00e1lcico; a su vez, los \u00e1cidos n\u00edtrico y fosf\u00f3rico originan nitratos y fosfatos c\u00e1lcicos.<\/p>\n\n\n\n

    \"
    Tierras calizas<\/p>\n\n\n\n

    Todos estos elementos pueden ser absorbidos por las plantas, aunque un exceso de cal s\u00f3lo es soportado por las plantas calc\u00edcolas. Otra presencia en el suelo \u00fatil para las plantas es la dolom\u00eda (CaMg(CO3)2), carbonato doble de calcio y magnesio, que sintetiza la clorofila.<\/p>\n\n\n\n

    \u00d3xidos de hierro<\/h2>\n\n\n\n

    \"
    \u00d3xidos de hierro<\/p>\n\n\n\n

    Los \u00f3xidos e hidr\u00f3xidos de hierro (oligisto y limonita) se producen como resultado de la meteorizaci\u00f3n de la mica negra (biotita) y otros silicatos (anfiboles y piroxenos). Estos elementos son los causantes de que las tierras presenten colores rojos y amarillos.<\/p>\n\n\n\n

    \"
    \u00cdndice Ecolog\u00eda<\/span><\/a> <\/p>\n","protected":false},"excerpt":{"rendered":"

    e puede dividir la composici\u00f3n qu\u00edmica de los suelos en org\u00e1nicos e inorg\u00e1nicos. Representan las part\u00edculas minerales el 50% del total, de las cuales dominan la arena, arcilla y caliza, y en menor medida \u00f3xidos e hidr\u00f3xidos de hierro y sales; las de origen org\u00e1nico suponen el 5%; el 45%…<\/p>\n

    Seguir leyendo…<\/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":[77,4,5,38,78,73],"class_list":["post-421","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-ecologia","tag-composicion","tag-ecologia","tag-general","tag-parte","tag-quimica","tag-suelo"],"yoast_head":"\nECOLOG\u00cdA GENERAL - EL SUELO: COMPOSICI\u00d3N QU\u00cdMICA - 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-composicion-quimica-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: COMPOSICI\u00d3N QU\u00cdMICA - 1\u00aa PARTE - Aula de Naturaleza educativa\" \/>\n<meta property=\"og:description\" content=\"e puede dividir la composici\u00f3n qu\u00edmica de los suelos en org\u00e1nicos e inorg\u00e1nicos. 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