Journal
JOURNAL OF HAZARDOUS MATERIALS
Volume 300, Issue -, Pages 329-337Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.jhazmat.2015.07.009
Keywords
Algae decomposition; Diffusive gradients in thin-films (DGT); Phosphorus-iron-sulfur (P-Fe-S); Lake taihu; Sediment-water interface (SWI)
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Funding
- National Natural Science Funds for Distinguished Young Scholars [41322011]
- National Science Foundation of China [41403097, 21177134]
- Jiangsu Natural Science Foundation [BK20141060]
- Nanjing Institute of Geography and Limnology, CAS [NIGLAS2013QD04]
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This study addresses the previously unknown effects of algae blooms on the dynamics of phosphorus (P), iron (Fe) and sulfur (S) across a lacustrine sediment-water interface (SWI). A mesocosm experiment was conducted in-situ to investigate these effects based on two recently-developed diffusive gradients in thin-films techniques (DGT). Soluble P, Fe(II), and S(-II) exhibited similar changing trends in a water column subject to the algae addition. Peak concentrations appeared on day 7 of the 16-day experiment. The lowest Eh occurred at the experiment's midway point indicating a strong algae degradation. A maximum increase in DGT-labile S appeared on day 8 near the SW!, while the DGT-labile P and Fe exhibited persistent increases almost to the end of experiment. Significantly positive correlations of labile P were observed switching from between labile Fe and labile S in sediments, suggesting a significant change in original Fe-coupled dynamics of P under algae decomposition. Apparent fluxes were calculated based on DGT profiles where a simultaneous release of P and S occurred from degraded algae, resulting in bidirectional diffusion fluxes from sediment to overlying water. In contrast, sediment acted as a major source of labile Fe due to added depth and apparently positive fluxes. (C) 2015 Elsevier B.V. All rights reserved.
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