Mobility of Phosphorus during the Weathering of Volcanic Ashes
Data are presented on phosphorus mobility during the weathering of rhyolite-dacite tephra of the modern and ancient eruptions. Distal tephra cannot be considered a phosphorus source, since phosphorous has low mobility during weathering both in subaerial and subaqueous sedimentation conditions. Howev...
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Veröffentlicht in: | Lithology and Mineral Resources 2002-05, Vol.37 (3), p.275-278 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | Data are presented on phosphorus mobility during the weathering of rhyolite-dacite tephra of the modern and ancient eruptions. Distal tephra cannot be considered a phosphorus source, since phosphorous has low mobility during weathering both in subaerial and subaqueous sedimentation conditions. However, volcanic ashes exert a fertilization effect, providing the supply of nutrient elements into the ecosystem of internal basins and coastal zones.[PUBLICATION ABSTRACT] |
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ISSN: | 0024-4902 1573-8892 1608-3229 |
DOI: | 10.1023/A:1015490415475 |