Phosphorus distribution in the sediments of a shallow eutrophic lake, Lake Chaohu, China
In this study, the sediment profiles of total phosphorus (TP), inorganic phosphorus (P i ), organic phosphorus (P o ), C/P and N/P were used to investigate time-dependent P distribution changes in Lake Chaohu. The characteristics of P i and P o fractions in the surface sediments were studied and the...
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Veröffentlicht in: | Environmental earth sciences 2011-04, Vol.62 (8), p.1643-1653 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | In this study, the sediment profiles of total phosphorus (TP), inorganic phosphorus (P
i
), organic phosphorus (P
o
), C/P and N/P were used to investigate time-dependent P distribution changes in Lake Chaohu. The characteristics of P
i
and P
o
fractions in the surface sediments were studied and the difference between east and west lake region was also discussed. The P
i
and P
o
contents displayed a clear gradient from east to west in sediments of Lake Chaohu, and the P
o
/P ratios were lower in sediments with industrial and urban pollution sources input in west lake region. The study indicated that different sediments area had diverse concentrations and distributions of P
o
fractions due to their different drainage basin and pollution sources. The profile distribution of the C/P and N/P ratios decreased with increasing depths and stayed relatively constant ratios at the depths of 15–30 cm. The C/P and N/P ratios were always below Redfield ratios in sediment profile, indicating P enrichment but likely due to the preferential loss of carbon in respect to phosphorus. The rank order of P
i
-fractions extracted was HCl-P
i
> NaOH-P
i
> NaHCO
3
-P
i
in surface sediments. The relative distribution of NaHCO
3
-P
i
and HCl-P
i
was in agreement with the trophic conditions of the regions studied. Among the sequentially extracted P
o
forms, the rank order of P
o
fractions was residual P
o
> HCl-P
o
> fulvic acid-P > humic acid-P > NaHCO
3
-P
o
, with mean relative proportion of 5.4:3.4:2.2:1.1:1.0. |
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ISSN: | 1866-6280 1866-6299 |
DOI: | 10.1007/s12665-010-0649-5 |