College of Environmental Science and Technology, Yangzhou University, Yangzhou, 225217, China.
State Key Laboratory of Environment Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, China.
Environ Pollut. 2018 Jun;237:166-173. doi: 10.1016/j.envpol.2018.02.048. Epub 2018 Feb 24.
Nitrogen pollution has become a worldwide problem and the source identification is important for the development of pertinent control measures. In this study, isotope end members (rain, nitrogen fertilizer, untreated/treated sewage), and samples (river water discharging to Taihu lake, lake water, aquatic organisms of different trophic levels) were taken during 2010-2015 to examine their δN values and nutrient stoichiometry. Results indicated that phytoplankton (primary producers), which directly take up and incorporate N from the lake water, had a similar δN value (14.1‰ ± 3.2) to the end member of treated sewage (14.0‰ ± 7.5), and the most frequently observed δN value in the lake water was 8-12‰, both indicating the dominant impact of the sewage discharge. Relationship analysis between N isotope value of nitrate and nitrate concentration indicated that different N cycling existed between the algae-dominated northwest lake (NW) and the macrophyte-dominated southeast lake (SE), which is a result of both impacts of river inputs and denitrification. Our nutrient stoichiometry analysis showed that the lake water had a significantly higher N:P ratio than that of algae (p < 0.05), suggesting that N is available in excess relative to the amount demanded by the algae. The long-term trend of the socio-economic development in the watershed further confirmed that the rapid population increase and urbanization have resulted in a great change in the N loading and source proportion. We suggest that although P control is necessary in terms of eutrophication control, N pollution control is urgent for the water quality and ecological recovery for Taihu lake.
氮污染已成为全球性问题,识别污染源对于制定相关控制措施至关重要。本研究于 2010-2015 年采集了同位素端元(雨水、化肥、未经处理/处理后的污水)和样本(排入太湖的河水、湖水、不同营养级别的水生生物),以检测其δN 值和养分化学计量。结果表明,直接从湖水中吸收和同化 N 的浮游植物(初级生产者)的δN 值(14.1‰±3.2)与处理后污水的端元(14.0‰±7.5)相似,而湖中最常见的δN 值为 8-12‰,均表明污水排放的主要影响。硝酸盐氮同位素值与硝酸盐浓度的关系分析表明,藻类占优势的西北湖区(NW)和大型植物占优势的东南湖区(SE)之间存在不同的氮循环,这是河流输入和反硝化作用的共同影响所致。我们的养分化学计量分析表明,湖水的 N:P 比值明显高于藻类(p<0.05),表明相对于藻类的需求,N 的供应过剩。流域社会经济发展的长期趋势进一步证实,人口的快速增长和城市化导致了氮负荷和来源比例的巨大变化。我们建议,尽管从富营养化控制的角度来看,P 控制是必要的,但对于太湖的水质和生态恢复,氮污染控制迫在眉睫。