{"id":334,"date":"2021-11-11T18:00:46","date_gmt":"2021-11-11T17:00:46","guid":{"rendered":"https:\/\/www.humus-form.eu\/?page_id=334"},"modified":"2023-08-24T16:28:52","modified_gmt":"2023-08-24T14:28:52","slug":"gliederung-der-of-horizonte","status":"publish","type":"page","link":"https:\/\/www.humus-form.eu\/?page_id=334","title":{"rendered":"Of-horizons"},"content":{"rendered":"<p><strong>Olf<br \/>\n<\/strong>Of transition horizon (Ol-Of), in which the macroscopically detectable needle and leaf debris predominates over the organic fine matter (Figure 7b).<br \/>\n[l from <strong>l<\/strong>itter]<\/p>\n<ol>\n<li>organic carbon content \u2265 15 mass % and<\/li>\n<li>developed under aeromorphic to aero-hydromorphic conditions<\/li>\n<li>Proportion of organic fine matter 10 &#8211; &lt; 30 vol.%<\/li>\n<\/ol>\n<p>&nbsp;<\/p>\n<blockquote>\n<div id=\"attachment_744\" style=\"width: 310px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/12\/Pilzhyphen-im-Of-02.jpg\"><img aria-describedby=\"caption-attachment-744\" decoding=\"async\" loading=\"lazy\" class=\"wp-image-744 size-medium\" src=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/12\/Pilzhyphen-im-Of-02-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/12\/Pilzhyphen-im-Of-02-300x225.jpg 300w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/12\/Pilzhyphen-im-Of-02-768x576.jpg 768w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/12\/Pilzhyphen-im-Of-02-400x300.jpg 400w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/12\/Pilzhyphen-im-Of-02.jpg 850w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-744\" class=\"wp-caption-text\">Olf horizont, leaf material: common beech (Fagus sylvatica) with fungus mycelium,\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0\u00a0 \u00a9 Jan Evers<\/p><\/div><\/blockquote>\n<p><a href=\"https:\/\/www.humus-form.eu\/?page_id=472\" rel=\"noopener\">(-&gt; L Mull-like F Mull)<\/a><\/p>\n<p><strong>Ohf<br \/>\n<\/strong>Of transition horizon (Oh-Of) with a high to predominant proportion of organic fine matter and lower proportions of macroscopically recognisable remains of dead plant biomass\/litter (Figure 7c).<br \/>\n[h from <strong>h<\/strong>umified]<\/p>\n<ol>\n<li>organic carbon content \u2265 15 mass % and<\/li>\n<li>developed under aeromorphic to aero-hydromorphic conditions<\/li>\n<li>Proportion of organic fine matter 30 &#8211; &lt; 70 vol.%<\/li>\n<\/ol>\n<blockquote>\n<div id=\"attachment_40\" style=\"width: 310px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Beprobung-03.jpg\"><img aria-describedby=\"caption-attachment-40\" decoding=\"async\" loading=\"lazy\" class=\"wp-image-40 size-medium\" src=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Beprobung-03-300x224.jpg\" alt=\"\" width=\"300\" height=\"224\" srcset=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Beprobung-03-300x224.jpg 300w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Beprobung-03-1024x766.jpg 1024w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Beprobung-03-768x575.jpg 768w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Beprobung-03-1536x1149.jpg 1536w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Beprobung-03-2048x1532.jpg 2048w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Beprobung-03-401x300.jpg 401w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-40\" class=\"wp-caption-text\">Ohf horizon, leaf material: common beech (Fagus sylvatica) \u00a9 Gerhard Milbert<\/p><\/div><\/blockquote>\n<p style=\"text-align: center;\" data-wp-editing=\"1\">Ohf horizont, leaf material: common beech (F<em>agus sylvatica<\/em>)<br \/>\n\u00a9 Gerhard Milbert<\/p>\n<p data-wp-editing=\"1\"><a href=\"https:\/\/www.humus-form.eu\/?page_id=478\" rel=\"noopener\">(-&gt; Moder-like F-Mull)<\/a><\/p>\n<p><strong>Odf<br \/>\n<\/strong>Of modified horizon with root felt.<br \/>\n[d from &#8222;stark <strong>d<\/strong>urchwurzelt&#8220; (german for strong rooting)]<\/p>\n<ol>\n<li>organic carbon content \u2265 15 mass % and<\/li>\n<li>developed under aeromorphic to aero-hydromorphic conditions<\/li>\n<li>Proportion of living fine roots \u2265 50 vol.%<\/li>\n<\/ol>\n<p><a href=\"https:\/\/www.humus-form.eu\/?page_id=476\" rel=\"noopener\">(-&gt; Rhizo F Mull)<\/a><\/p>\n<p><strong>Owf<br \/>\n<\/strong>Of modified horizon, temporarily influenced by stagnic water or groundwater. Vegetation indicates wetness in the A horizon (Figure 14).<br \/>\n[w from <strong>w<\/strong>ater influenced]<\/p>\n<ol>\n<li>organic carbon content \u2265 15 mass % and<\/li>\n<li>developed under aeromorphic to aero-hydromorphic conditions<\/li>\n<li>Proportion of living fine roots \u2265 50 vol.%<\/li>\n<li>temporarily anaerobic conditions and<\/li>\n<li>grey to black colouring of the litter and<\/li>\n<li>above recently water influenced hydromorphic A or H horizon<\/li>\n<\/ol>\n<p><a href=\"https:\/\/www.humus-form.eu\/?page_id=480\" rel=\"noopener\">(<em>-&gt;Moist F Mull<\/em>)<\/a><\/p>\n<div id=\"attachment_48\" style=\"width: 310px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Feuchtmull-scaled.jpg\"><img aria-describedby=\"caption-attachment-48\" decoding=\"async\" loading=\"lazy\" class=\"wp-image-48 size-medium\" src=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Feuchtmull-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Feuchtmull-300x225.jpg 300w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Feuchtmull-1024x768.jpg 1024w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Feuchtmull-768x576.jpg 768w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Feuchtmull-1536x1152.jpg 1536w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Feuchtmull-2048x1536.jpg 2048w, https:\/\/www.humus-form.eu\/wp-content\/uploads\/2021\/11\/Feuchtmull-400x300.jpg 400w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-48\" class=\"wp-caption-text\">Ol-horizon, leaf material: common oak (Quercus robur) on top of a hydromorphic\u00a0 Owf horizon,<br \/>\u00a9 Gerhard Milbert<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Olf Of transition horizon (Ol-Of), in which the macroscopically detectable needle and leaf debris predominates over the organic fine matter (Figure 7b). [l from litter] organic carbon content \u2265 15 mass % and developed under aeromorphic to aero-hydromorphic conditions Proportion &hellip; <a href=\"https:\/\/www.humus-form.eu\/?page_id=334\">Weiterlesen <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":148,"menu_order":2,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v20.11 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Of-horizons - Humus Form<\/title>\n<meta name=\"description\" content=\"Of, Olf, Ohf, Owf, Odf, Streu zerkleinert, fragmentiert, rudimentiert, skelettiert, geringer bis mittlerer Grd der Humifizierung, organische Feinsubstand 10 - 20 Volumen-%, Lagerungsform der Streu locker bis stark verfilzt\" \/>\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=334\" \/>\n<meta property=\"og:locale\" content=\"de_DE\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Of-horizons - 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