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File:Kaltenhofer Moor Vernässungsfläche.jpg

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Deutsch: Hochmoor Die Hochmoore in Schleswig-Holstein sind nach der letzten Eiszeit entstanden. Voraus-setzung für ihr Wachstum ist, dass die Nieder-schlagsmenge größer ist als der Wasserverlust durch Verdunstung oder Abfluss.„Baumeister“ der Hochmoore sind verschie-dene Torfmoosarten der Gattung Sphagnum.Torfmoose haben keine Wurzeln. Während sie nach oben unbegrenzt wachsen, sterben sie nach unten hin ab. Aufgrund des Sau-erstoffmangels werden aber die anfallenden Pflanzenreste nicht zersetzt, sondern als Torf abgelagert. Der Moorkörper wächst so mit einer Geschwindigkeit von etwa 1 mm pro Jahr langsam in die Höhe. Seine Oberfläche ist in Bulte und Schlenken gegliedert, wo jeweils unterschiedliche Torfmoose wachsen. Ungestörte Hochmoore sind „wachsende“ Böden.
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current13:13, 4 May 2019Thumbnail for version as of 13:13, 4 May 20195,227 × 3,545 (13.64 MB)S.N-Foto (talk | contribs)User created page with UploadWizard

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