

FOLLOWUS
1.State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
2.School of Oceanography, Shanghai Jiao Tong University, Shanghai 200240, China
Shan JIANG, E-mail: sjiang@sklec.ecnu.edu.cn
收稿:2020-04-07,
录用:2020-5-18,
网络首发:2020-07-14,
纸质出版:2021-05
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Nitrate in the Changjiang diluted water: an isotopic evaluation on sources and reaction pathways[J]. 海洋湖沼学报(英文), 2021,39(3):830-845.
Shan JIANG, Jie JIN, Guosen ZHANG, et al. Nitrate in the Changjiang diluted water: an isotopic evaluation on sources and reaction pathways[J]. Journal of Oceanology and Limnology, 2021, 39(3): 830-845.
Nitrate in the Changjiang diluted water: an isotopic evaluation on sources and reaction pathways[J]. 海洋湖沼学报(英文), 2021,39(3):830-845. DOI: 10.1007/s00343-020-0149-8.
Shan JIANG, Jie JIN, Guosen ZHANG, et al. Nitrate in the Changjiang diluted water: an isotopic evaluation on sources and reaction pathways[J]. Journal of Oceanology and Limnology, 2021, 39(3): 830-845. DOI: 10.1007/s00343-020-0149-8.
A cruise covering two transects in the Changjiang (Yangtze) estuary in July 2017 was conducted
aiming to explore the sources for riverine NO
3
-
and identify reactions involved in the NO
3
-
transformations along the transport of the Changjiang diluted water (CDW). In the river water
NO
3
-
was fundamentally contributed by chemical fertilizer leakage in the watershed according to isotope signals. Sewage discharge may also be significant on riverine NO
3
-
inventory
while the isotope signal was masked by nitrification. Together with the transport of the CDW
NO
3
-
production was observed in waters with low salinities (
<
20) and high turbidities. Nitrification resulted from the mineralization of riverine organic nitrogen; therefore
the high turbidity was linked to active production. In the outer plume
coupled with stratification
a significant decrease in NO
3
-
concentration was observed in the surface water. In parallel
enrichment in δ
15
N-NO
3
-
and δ
18
O-NO
3
-
was found
indicating biological consumption by phytoplankton. The difference in the stratification intensity between two transects led to variations in NO
3
-
concentrations and isotope compositions. In the benthic water
denitrification (sediment-water interface) and nitrification (bottom water) coexisted. Furthermore
accumulations of NH
4
+
and dissolved organic nitrogen in the bottom water were observed
indicating that nitrification was constrained by oxidant (mainly dissolved oxygen) supplies.
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