Zheng Bing-Hui, Cao Cheng-Jin, Qin Yan-Wen, Huang Min-Sheng
River and Coastal Environment Research Center, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
Huan Jing Ke Xue. 2008 Jan;29(1):1-6.
According to the survey conducted from Jan. 2004 to Dec. 2005, the seasonal characters of nitrogen in the water of input rivers of Three Gorges Reservoir (TGR) were discussed, and the forms and distributions of nitrogen among three major input rivers (Changjiang river, Jialingjiang river and Wujiang river) were studied. The results indicate that some primary hydrologic values of input rivers have seasonal characters, and they are in the danger range, which might bring algal bloom. The average contents per year of total nitrogen are 1.55-2.15 mg/L in the three monitor sections of input rivers of TGR, and Wulong monitor section is more severe than the others. The contents of total nitrogen in abundant water period are much higher than them in low water period, which displays the nonpoint source pollution has far-reaching influence upon total nitrogen. The total dissolved inorganic nitrogen (DIN) is the major form of total nitrogen and further nitrate nitrogen (NO3(-)-N) is dominant accounting for 70% or more of DIN. Ammoniacal nitrogen is the uppermost input form of nitrogen pollution of input rivers of TGR. Ammoniacal nitrogen was oxidated to nitroso-nitrogen, and then it was oxidated to nitrate nitrogen using up a lot of dissolved oxygen of water. Nitrate nitrogen sources include agricultural runoff, city pollution water, city runoff and slow-releasing from submersed soil, whenas nitrogen-ammonia (NH4(+)-N) origins are city pollution water, industrial pollution water, and a little source of living garbage and bilgewater.
根据2004年1月至2005年12月进行的调查,探讨了三峡水库入库河流中氮的季节特征,并研究了氮在三条主要入库河流(长江、嘉陵江和乌江)中的形态和分布。结果表明,入库河流的一些主要水文值具有季节特征,且处于可能引发藻类大量繁殖的危险范围内。三峡水库入库河流三个监测断面的总氮年均含量为1.55 - 2.15mg/L,其中武隆监测断面情况更为严峻。丰水期总氮含量远高于枯水期,这表明面源污染对总氮影响深远。总溶解无机氮(DIN)是总氮的主要形态,其中硝酸盐氮(NO3(-)-N)占DIN的70%以上,占主导地位。氨氮是三峡水库入库河流氮污染的最主要输入形态。氨氮先被氧化为亚硝酸盐氮,进而氧化为硝酸盐氮,消耗了大量水体中的溶解氧。硝酸盐氮来源包括农业径流、城市污水、城市径流以及淹没土壤的缓慢释放,而氨氮(NH4(+)-N)来源为城市污水、工业污水以及少量生活垃圾和舱底水。