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Mikrobiologie und Ökophysiologie des Stickstoffkreislaufs

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Mikrobiologie von Böden

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Zusammenfassung

In Atmosphäre, Böden und Gewässern der Erde befinden sich ca. 4 × 1021 g N (= 4 × 1015 t N = 4 Pt N) im Umlauf, allerdings liegen mehr als 99% davon in Form von atmosphärischem N2 vor. Im N-Kreislauf unseres Planeten sind weniger als 0,1% des Gesamt-N-Gehalts organisch gebunden, im Wesentlichen in den terrestrischen Ökosystemen. In diesen Ökosystemen, einschließlich Pflanzen, Tieren und Mikroorganismen, sind global etwa 332–350 Pg N (1 Pg = 1015 g) enthalten. Sedimente, Steinkohle und Gesteine speichern zusätzlich noch ca. 2 × 1018 g N. In den terrestrischen Ökosystemen verteilen sich ungefähr 88–100 Pg N auf organisch gebundenen N in Ah- und Ap-Horizonten von Böden, ca. 2,0 Pg N auf die Streuauflagen (O-Horizonte), etwa 10–13 Pg N auf die pflanzliche und ca. 0,2 Pg N auf die tierische Biomasse. Etwa 2 Pg N befinden sich global in der mikrobiellen Biomasse von Böden (Batjes 1996). Die Mengen an tonmineralfixiertem NH4 +-N in Böden werden global auf 20 Pg N geschätzt.

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  1. Institut für Angewandte Mikrobiologie, Justus Liebig-Universität, Heinrich-Buff-Ring 26–32, 35392, Gießen, Deutschland

    Professor em. Dr. sc. agr. habil. Johannes C. G. Ottow

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  1. Professor em. Dr. sc. agr. habil. Johannes C. G. Ottow
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Ottow, J. (2011). Mikrobiologie und Ökophysiologie des Stickstoffkreislaufs. In: Mikrobiologie von Böden. Springer-Lehrbuch. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-00824-5_12

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