Effect of enhanced reactive nitrogen availability on plant-sediment mediated degradation of polycyclic aromatic hydrocarbons in contaminated mangrove sediment

As land–ocean interaction zones, mangrove systems receive substantial polycyclic aromatic hydrocarbons (PAHs) from sewage and combustion of fossil fuel. In this study, we investigated the relationship between dissolved inorganic nitrogen (DIN) availability and degradation rate of phenanthrene, a typ...

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Veröffentlicht in:Marine pollution bulletin 2016-02, Vol.103 (1-2), p.151-158
Hauptverfasser: Jiang, Shan, Lu, Haoliang, Zhang, Qiong, Liu, JingChun, Yan, Chongling
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Sprache:eng
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Zusammenfassung:As land–ocean interaction zones, mangrove systems receive substantial polycyclic aromatic hydrocarbons (PAHs) from sewage and combustion of fossil fuel. In this study, we investigated the relationship between dissolved inorganic nitrogen (DIN) availability and degradation rate of phenanthrene, a typical PAH compound, in mangrove plant-sediment systems, using Avicennia marina as a model plant. After 50day incubation, phenanthrene removal ratios in sediments ranged from 53.8% to 97.2%. In non-rhizosphere sediment, increasing DIN accessibility increased microbial biomass and total microbial activity, while enhancements in population size of phenanthrene degradation bacteria (PDB) and phenanthrene degradation rates were insignificant. In contrast, the presence of excessive DIN in rhizosphere sediment resulted in a significantly large number of PDB, leading to a rapid dissipation rate of phenanthrene. The differences in degradation rates and abundances of degrader in sediment may be explained by the enhanced root activity due to the elevation in DIN accessibility. •Introduction of dissolved inorganic nitrogen increased microbial biomass and activity in mangrove sediment.•Dissolved inorganic nitrogen amendment could stimulate root activity of Avicennia marina (Forsk.) Vierh.•Enhancement in dissolved inorganic nitrogen availability increased phenanthrene degradation rates in rhizosphere sediment.
ISSN:0025-326X
1879-3363
DOI:10.1016/j.marpolbul.2015.12.027