A lab-scale study on heterotrophic nitrification-aerobic denitrification for nitrogen control in aquatic ecosystem
Nitrogen (N) loss is generally caused by denitrification under anaerobic conditions and the N loss in the heterotrophic nitrification _ aerobic denitrification (HN _ AD) system is of recent research interest. However, previous studies are generally focused on pure cultures-based system and the infor...
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Veröffentlicht in: | Environmental science and pollution research international 2020-03, Vol.27 (9), p.9307-9317 |
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Sprache: | eng |
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Zusammenfassung: | Nitrogen (N) loss is generally caused by denitrification under anaerobic conditions and the N loss in the heterotrophic nitrification
_
aerobic denitrification (HN
_
AD) system is of recent research interest. However, previous studies are generally focused on pure cultures-based system and the information on HN
_
AD in the complex aquatic ecosystem is limited. In this study, HN-AD system was established in the mixed cultures of the sediments and the performances of HN-AD were evaluated under different conditions. Further, the N loss mechanism in HN
_
AD system was explored. The study found that the N was lost in the sediment cultures with ammonium-N (NH
4
+_
N) (or) and nitrate-N (NO
3
−_
N) as N source under aerobic conditions. The highest N loss rate was achieved under the TOC/TN mass ratio of 10 with citrate as the carbon source. Under this condition, the N loss percentages of NH
4
+_
N (201.91 mg/L) and NO
3
−_
N (130.00 mg/L) reached 99.61% and 100.00%, respectively, which were higher than those in the pure HN
_
AD strains reported in the literature. High NH
4
+_
N removal efficiencies were also achieved at low C/N mass ratio and high NH
4
+_
N concentration (493.12 mg L
−1
). The N loss pathway in the system was investigated by adding Na
2
WO
4
as the nitrate reductase inhibitor. The study found that the N was not lost via partial nitrification/denitrification pathway, i.e., NH
4
+
→ NH
2
OH → NO
2
−
→ N
2
O (N
2
), instead via full nitrification/denitrification pathway, i.e., NH
4
+
→ NH
2
OH → NO
2
−
→ NO
3
−
→ NO
2
−
→ N
2
O (N
2
), since nitrate was a key intermediate. The variation in NH
4
+_
N, NO
3
−_
N, and NO
2
−_
N concentrations in the HN
_
AD processes further confirmed the N transformation pathway. Therefore, HN
_
AD may occur and cause N loss in natural aquatic ecosystems. The results of this study demonstrate that N was lost through HN-AD and that the well-cultured HN-AD sediments could be useful biological tool to remediate eutrophic water bodies. |
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ISSN: | 0944-1344 1614-7499 |
DOI: | 10.1007/s11356-019-07551-3 |