{"id":155,"date":"2021-11-07T17:49:52","date_gmt":"2021-11-07T16:49:52","guid":{"rendered":"https:\/\/www.humus-form.eu\/?page_id=155"},"modified":"2023-08-25T09:54:22","modified_gmt":"2023-08-25T07:54:22","slug":"e-horizonte","status":"publish","type":"page","link":"https:\/\/www.humus-form.eu\/?page_id=155","title":{"rendered":"E-horizons"},"content":{"rendered":"<p><strong>Ee<\/strong><\/p>\n<p>E horizon, podzolised, strongly lightened by translocation of iron (hydr)oxides and humus substances, acid bleached. Transition to the following horizon often cone- or tongue-shaped [e from <strong>e<\/strong>luviated].<\/p>\n<ol>\n<li>light, pale soil matrix and<\/li>\n<li>a) purplish or mottled by acid bleaching, or<br \/>\nb) bleached quartz grains and<\/li>\n<li>hardly any organic matter<\/li>\n<\/ol>\n<p><em>Note:<\/em><\/p>\n<ul>\n<li>prevalent Value \u2265 4 (dry \u2265 5) and Quotient Value and Chroma \u2265 2,5.<\/li>\n<li>mostly overlaying an\u00a0 Illuvialhorizont (such as.: Kh, Ksh, Ks or Ks-Bv Horizon)<em><br \/>\n<\/em><\/li>\n<\/ul>\n<blockquote>\n<div id=\"attachment_997\" style=\"width: 271px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2023\/07\/Rohhumus-06.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-997\" class=\"wp-image-997\" src=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2023\/07\/Rohhumus-06-206x300.jpg\" alt=\"\" width=\"261\" height=\"373\" \/><\/a><p id=\"caption-attachment-997\" class=\"wp-caption-text\">Stagnic Podzol, parent material\u00a0 glacial sand\u00a0 with a thick forest floor (Mor)<br \/>horizon sequence: Ol \/ Of \/ Osh \/ Ee \/ Khs \/ Sw (Thilo Simon, GD NRW)<\/p><\/div><\/blockquote>\n<p>&nbsp;<\/p>\n<p><strong>Ah-Ee<\/strong><\/p>\n<p>Ee transition horizon.<\/p>\n<ol>\n<li>light, pale soil matrix and<\/li>\n<li>acid bleached and<\/li>\n<li>organic carbon content \u2265 0.5 mass % and<\/li>\n<li>uneven proportion of humus, in the form of mottling and diffuse bleaching (partly mottled due to microbial decomposition) or due to accumulation of humus from the organic layer.<\/li>\n<\/ol>\n<p>&nbsp;<\/p>\n<p><strong>Ee-Ah<\/strong><\/p>\n<p>Ah transition horizon, weakly podzolised.<\/p>\n<ol>\n<li>acid bleached and<\/li>\n<li>under humus layer, thin, grey or black-grey coloured layer due to humus accumulation<\/li>\n<\/ol>\n<p>Note:<\/p>\n<ul>\n<li>prevalent soil colour: Hue 7,5YR to 2,5YR and Value \u2265 3 and \u2264 4.<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Ee E horizon, podzolised, strongly lightened by translocation of iron (hydr)oxides and humus substances, acid bleached. Transition to the following horizon often cone- or tongue-shaped [e from eluviated]. light, pale soil matrix and a) purplish or mottled by acid bleaching, &hellip; <a href=\"https:\/\/www.humus-form.eu\/?page_id=155\">Weiterlesen <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":109,"menu_order":4,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-155","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v28.2 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>E-horizons - Humus Form<\/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:\/\/www.humus-form.eu\/?page_id=155\" \/>\n<meta property=\"og:locale\" content=\"de_DE\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"E-horizons - Humus Form\" \/>\n<meta property=\"og:description\" content=\"Ee E horizon, podzolised, strongly lightened by translocation of iron (hydr)oxides and humus substances, acid bleached. 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