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 |
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Sprache: | eng |
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