{"id":109,"date":"2021-11-07T12:53:43","date_gmt":"2021-11-07T11:53:43","guid":{"rendered":"https:\/\/www.humusformen.de\/?page_id=109"},"modified":"2023-09-13T15:30:26","modified_gmt":"2023-09-13T13:30:26","slug":"horizontdefinitionen-der-humusformen-relevanten-horizonte","status":"publish","type":"page","link":"https:\/\/www.humusformen.de\/?page_id=109","title":{"rendered":"Horizonte"},"content":{"rendered":"\r\n<p class=\"has-medium-font-size\"><strong>Definition der humusformenrelevanten Horizonte<\/strong><\/p>\r\n<p><a title=\"O-Horizont\" href=\"https:\/\/www.humusformen.de\/?page_id=148\"><strong>O-Horizont<\/strong><\/a><\/p>\r\n<div class=\"wp-block-column\">Organischer Haupt-Horizont, entstanden unter aeromorphen bis aero-hydromorphen Bedingungen an der Bodenoberfl\u00e4che aus abgestorbener Biomasse (vor allem Pflanzenstreu) [O von organisch].<\/div>\r\n<div>\u00a0<\/div>\r\n<ol>\r\n<li>Anteil organischen Kohlenstoffs \u2265 15 Masse-% und<\/li>\r\n<li>unter aeromorphen bis aero-hydromorphen Bedingungen entstanden.<\/li>\r\n<\/ol>\r\n<blockquote>\r\n<div id=\"attachment_749\" style=\"width: 445px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/Typische-Moder-Horizonte.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-749\" class=\"wp-image-749\" src=\"https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/Typische-Moder-Horizonte-300x194.jpg\" alt=\"\" width=\"435\" height=\"288\" \/><\/a><p id=\"caption-attachment-749\" class=\"wp-caption-text\">Ol\/Olf\/Ohf\/Obh1 (rotbraun)\/Obh2 (schwarz)\/Ah-Ee\/Ee -Horizontfolge aus Buchenstreu-Auflage und Flugsand, \u00a9 Geologischer Dienst NRW<\/p><\/div>\r\n<\/blockquote>\r\n<div><a href=\"https:\/\/www.humusformen.de\/?page_id=153\"><strong>H-Horizont<\/strong><\/a><\/div>\r\n<div>Organischer Horizont, der prim\u00e4r durch Torfbildung aus Resten torfbildender Pflanzen an der Gel\u00e4ndeoberfl\u00e4che unter topogenem oder ombrogenem Wasser\u00fcberschuss entstanden ist. Durch Entw\u00e4sserung und landwirtschaftliche Bewirtschaftung k\u00f6nnen H-Horizonte aerob sekund\u00e4r pedogen ver\u00e4ndert sein (Hm, Hv, Ha, Ht), nach Wiedervern\u00e4ssung k\u00f6nnen diese Horizonte als reliktische Horizonte auftreten [H von humifiziert].<\/div>\r\n<div>\r\n<ol>\r\n<li>Gehalt an organischem Kohlenstoff \u2265 15 Masse-% und<\/li>\r\n<li>aus Resten torfbildender Pflanzen entstanden<\/li>\r\n<\/ol>\r\n<blockquote>\r\n<div id=\"attachment_741\" style=\"width: 336px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/oligotrophes-H-Moor.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-741\" class=\"wp-image-741\" src=\"https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/oligotrophes-H-Moor-224x300.jpg\" alt=\"\" width=\"326\" height=\"431\" \/><\/a><p id=\"caption-attachment-741\" class=\"wp-caption-text\">Niedermoor in einem Zufluss zur Eder, Sauerland, sickernasser Quellbereich, nHhn-Horizont, \u00a9 Geologischer Dienst NRW<\/p><\/div>\r\n<p>&nbsp;<\/p>\r\n<p>&nbsp;<\/p>\r\n<\/blockquote>\r\n<\/div>\r\n<div>\u00a0<\/div>\r\n<p><a title=\"A-Horizont\" href=\"https:\/\/www.humusformen.de\/?page_id=150\"><strong>A-Horizont<\/strong><\/a><\/p>\r\n<div class=\"wp-block-column is-vertically-aligned-top\">Dunkel gef\u00e4rbter mineralischer Oberbodenhorizont mit Akkumulation von in situ entstandener organischer Substanz, zu der auch organische D\u00fcngung oder frische Sedimentation beigetragen haben k\u00f6nnen. Die organische Substanz ist in der Regel durch Wurzeln, Bioturbation, Pflug- oder Grabet\u00e4tigkeit, in versauerten B\u00f6den unter Humusauflage auch durch Einwaschung gel\u00f6ster organischer Substanz in den Boden gelangt. Merkmale der Unterbodenhorizonte nicht oder nur schwach vorhanden.<\/div>\r\n<div class=\"wp-block-column\">\r\n\r\nDer Horizont kann auch nach Entw\u00e4sserung aus einem U- oder H-Horizont entstanden sein, bei dem der Abbau der organischen Substanz gegen\u00fcber der Akkumulation neuer organischer Substanz \u00fcberwiegt oder bei dem durch Mischung (Pflugt\u00e4tigkeit und Moormelioration) mit mineralischen Substraten der Gehalt an organischer Substanz abnimmt.<\/div>\r\n<div>\u00a0<\/div>\r\n<ol>\r\n<li><em>Oberbodenhorizont mit erkennbarem Gehalt an organischer Substanz und <\/em><\/li>\r\n<li><em>Gehalt an organischem Kohlenstoff &lt; 15 Masse-% und <\/em><\/li>\r\n<li><em>mit Akkumulation von in-situ entstandener organischer Substanz, die z. T. auch aus organischer D\u00fcngung oder frischer Sedimentation stammen kann.<\/em><\/li>\r\n<\/ol>\r\n<p>&nbsp;<\/p>\r\n<div id=\"attachment_753\" style=\"width: 255px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/feinhumusarmer-F-Mull-aus-Buchenstreu-auf-Kalkstein-Verwitterungslehm.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-753\" class=\"wp-image-753 size-medium\" src=\"https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/feinhumusarmer-F-Mull-aus-Buchenstreu-auf-Kalkstein-Verwitterungslehm-245x300.jpg\" alt=\"\" width=\"245\" height=\"300\" srcset=\"https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/feinhumusarmer-F-Mull-aus-Buchenstreu-auf-Kalkstein-Verwitterungslehm-245x300.jpg 245w, https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/feinhumusarmer-F-Mull-aus-Buchenstreu-auf-Kalkstein-Verwitterungslehm-835x1024.jpg 835w, https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/feinhumusarmer-F-Mull-aus-Buchenstreu-auf-Kalkstein-Verwitterungslehm-768x941.jpg 768w, https:\/\/www.humusformen.de\/wp-content\/uploads\/2021\/12\/feinhumusarmer-F-Mull-aus-Buchenstreu-auf-Kalkstein-Verwitterungslehm.jpg 1240w\" sizes=\"(max-width: 245px) 100vw, 245px\" \/><\/a><p id=\"caption-attachment-753\" class=\"wp-caption-text\">Feinhumusarmer F-Mull aus Buchenlaubstreu \u00fcber Kalksteinverwitterung mit Ax-Horizont,<br \/>\u00a9 Christine Wachendorf, AG Humusformen<\/p><\/div>\r\n<blockquote>\r\n<p style=\"text-align: center;\">\u00a0<\/p>\r\n<\/blockquote>\r\n<p>&nbsp;<\/p>\r\n<p><a title=\"E-Horizonte\" href=\"https:\/\/www.humusformen.de\/?page_id=155\" rel=\"nofollow \"><strong>E-Horizont<\/strong><\/a><\/p>\r\n<p>Mineralischer Horizont, durch Verlagerung von Tonmineralen, Eisen(hydr)oxiden oder Humus verarmt [E von eluiert].<\/p>\r\n\r\n\r\n\r\n\r\n\r\n\r\n\r\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-layout-1 wp-block-columns-is-layout-flex\">\r\n<div class=\"wp-block-column\" style=\"flex-basis: 66.66%;\"><br \/><\/div>\r\n<!-- \/wp:column --><\/div>\r\n<!-- \/wp:columns -->\r\n\r\n<!-- wp:columns -->\r\n<div class=\"wp-block-columns\"><!-- wp:column {\"width\":\"33.33%\"} -->\r\n<div class=\"wp-block-column\" style=\"flex-basis: 33.33%;\"><!-- wp:paragraph --><\/div>\r\n<\/div>\r\n<p>&nbsp;<\/p>\r\n<!-- \/wp:paragraph -->","protected":false},"excerpt":{"rendered":"<p>Definition der humusformenrelevanten Horizonte O-Horizont Organischer Haupt-Horizont, entstanden unter aeromorphen bis aero-hydromorphen Bedingungen an der Bodenoberfl\u00e4che aus abgestorbener Biomasse (vor allem Pflanzenstreu) [O von organisch]. \u00a0 Anteil organischen Kohlenstoffs \u2265 15 Masse-% und unter aeromorphen bis aero-hydromorphen Bedingungen entstanden. H-Horizont &hellip; <a href=\"https:\/\/www.humusformen.de\/?page_id=109\">Weiterlesen <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":2,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v21.7 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Horizonte - Humusformen<\/title>\n<meta name=\"description\" content=\"O-Horizonte, H-Horizonte, A-Horizonte, E-HorizonteOl, Owl, Of, Olf, Ohf, Owf, Oh, Oih, Obh, Oxh, Ovh, Okh, Osh, Owbh, Ai, Ah, Ax, Au, Ee\" \/>\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.humusformen.de\/?page_id=109\" \/>\n<meta property=\"og:locale\" content=\"de_DE\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Horizonte - 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