Nie Bei, Zeng Yuhong, Niu Lanhua, Zhang Xiaofeng
State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, 430072, Wuhan, China.
Three Gorges Bureau of Hydrological and Water Resources Survey, Changjiang Water Resources Commission of the Ministry of Water Resources, Yichang, 443000, China.
Environ Sci Pollut Res Int. 2021 Dec;28(46):65633-65643. doi: 10.1007/s11356-021-15557-z. Epub 2021 Jul 28.
Nitrogen (N) is an essential nutrient limiting life, and its biochemical cycling and distribution in rivers have been markedly affected by river engineering construction and operation. Here, we comprehensively analyzed the spatiotemporal variations and driving environmental factors of N distributions based on the long-term observations (from 2004 to 2016) of seven stations in the Three Gorges Reservoir (TGR). In the study period, several water quality indexes of the river reach improved, whereas N pollution was severe and tended to be aggravated after the TGR impoundment. The anti-seasonal reservoir operation strongly affected the variations in N forms. The total nitrogen (TN) concentration in the mainstream of the Yangtze River continuously increased, although it was still lower than that in the incoming tributaries (Wu and Jialing rivers). Further analysis showed that this increase occurred probably because of external inputs, including the upstream (76%), non-point (22%), and point source pollution inputs (2%). Additionally, different N forms showed significant seasonal variations; among them, the TN and nitrate nitrogen concentrations were the lowest in the impoundment season (October-February), and the ammonia nitrogen concentrations were the highest in the sluicing season (March-May). Redundancy analysis revealed that the water level and distance to the Three Gorges Dam were significant contributors to N forms distribution. Our findings could provide a basis for managing and predicting the water quality in the Yangtze River.
氮(N)是限制生命的必需营养素,其在河流中的生物地球化学循环和分布受到河流工程建设和运行的显著影响。在此,我们基于三峡水库(TGR)七个站点的长期观测数据(2004年至2016年),全面分析了氮分布的时空变化及驱动环境因素。在研究期间,该河段的几个水质指标有所改善,然而氮污染严重,且在三峡水库蓄水后有加剧趋势。水库的反季节运行强烈影响了氮形态的变化。长江干流中的总氮(TN)浓度持续上升,尽管仍低于汇入支流(乌江和嘉陵江)中的浓度。进一步分析表明,这种增加可能是由于外部输入造成的,包括上游输入(76%)、非点源输入(22%)和点源污染输入(2%)。此外,不同的氮形态呈现出显著的季节变化;其中总氮和硝态氮浓度在蓄水季节(10月至次年2月)最低,氨氮浓度在泄水季节(3月至5月)最高。冗余分析表明,水位和距三峡大坝的距离是氮形态分布的重要影响因素。我们的研究结果可为长江水质管理和预测提供依据。