Tian Zebin, Zheng Binghui, Wang Lijing, Li Liqiang, Wang Xing, Li Hong, Norra Stefan
College of Water Sciences, Beijing Normal University, Beijing, China.
State Environmental Protection Key Laboratory of Drinking Water Source Protection, Chinese Research Academy of Environmental Sciences, Beijing, China.
PLoS One. 2017 Feb 6;12(2):e0170993. doi: 10.1371/journal.pone.0170993. eCollection 2017.
In order to protect the water quality of Dongting Lake, it is significant to find out its nitrogen pollution characteristics. Using long-term monthly to seasonally data (1997-2014), we investigated the spatial and temporal variations in nitrogen in Dongting Lake, the second largest freshwater lake in China. The average concentrations of total nitrogen (TN) in the eastern, southern, and western parts of the lake were 1.77, 1.56, and 1.35 mg/L, respectively, in 2014. TN pollution was generally worse in the southern area than in the western area. Concentrations showed temporal variation, and were significantly higher during the dry season than during the wet season. Based on the concentration and growth rate of TN, three different stages were identified in the long term lake data, from 1997 to 2002, from 2003 to 2008, and from 2009 to 2014, during which the concentrations and the growth rate ranged from 1.09-1.51 mg/L and 22.09%-40.03%, 1.05-1.57 mg/L and -9.05%-7.74%, and 1.68-2.02 mg/L and 57.99%-60.41%, respectively. The main controls on the lake water TN concentrations were the quality and quantity of the lake inflows, spatial and temporal variations in hydrodynamic conditions within the lake (flow velocity, flow direction), and point and nonpoint inputs from human activities. Diffuse nutrient losses from agricultural land are a significant contributor. As a priority, the local government should aim to control the pollutant inputs from upstream and non-point nutrient losses from land.
为保护洞庭湖水质,查明其氮污染特征具有重要意义。利用1997年至2014年长期的月度至季节性数据,我们对中国第二大淡水湖洞庭湖的氮时空变化进行了调查。2014年,洞庭湖东部、南部和西部的总氮(TN)平均浓度分别为1.77毫克/升、1.56毫克/升和1.35毫克/升。南部地区的TN污染总体上比西部地区更严重。浓度呈现出时间变化,旱季明显高于雨季。基于TN的浓度和增长率,在1997年至2002年、2003年至2008年以及2009年至2014年的长期湖泊数据中识别出三个不同阶段,在此期间,浓度和增长率分别为1.09 - 1.51毫克/升和22.09% - 40.03%、1.05 - 1.57毫克/升和 - 9.05% - 7.74%、1.68 - 2.02毫克/升和57.99% - 60.41%。湖水TN浓度的主要控制因素包括湖泊入流的质量和数量、湖内水动力条件(流速、流向)的时空变化以及人类活动的点源和非点源输入。农田的养分流失是一个重要因素。地方政府应优先控制上游的污染物输入和土地的非点源养分流失。