Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis

The long-term redistribution of Zn in a naturally Zn-enriched soil during pedogenesis was quantified based on mass balance calculations. According to their fate, parent limestones comprised three Zn pools: bound to calcite and pyrite-sphalerite grains, bound to phyllosilicates and bound to goethite...

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Veröffentlicht in:Pedosphere 2009-06, Vol.19 (3), p.292-304
Hauptverfasser: LAVEUF, C., CORNU, S., BAIZE, D., HARDY, M., JOSIERE, O., DROUIN, S., BRUAND, A., JUILLOT, F.
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Sprache:eng
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