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Abstract

Manganese occurs in various primary rocks and particularly in ferromagnesian materials. The Mn released from these rocks by weathering forms a number of secondary minerals the most prominent being pyrolusite (MnIVO2) and manganite [MnIIIO (OH)]. Manganese and Fe oxides often occur together in nodules and iron-pans. Total Mn levels may differ considerably between soils and are in a range from 20 to 3000 µg Mn/g (Gambrell 1996).

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Mengel, K., Kirkby, E.A., Kosegarten, H., Appel, T. (2001). Manganese. In: Mengel, K., Kirkby, E.A., Kosegarten, H., Appel, T. (eds) Principles of Plant Nutrition. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-1009-2_14

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  • DOI: https://doi.org/10.1007/978-94-010-1009-2_14

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