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京杭运河常州段氮形态的时空分布特征研究
引用本文:潘晨,陶玉炎,耿金菊,王荣俊,陈志宁,韩超,任洪强.京杭运河常州段氮形态的时空分布特征研究[J].环境科学与管理,2013(7):17-22.
作者姓名:潘晨  陶玉炎  耿金菊  王荣俊  陈志宁  韩超  任洪强
作者单位:[1]常州市环境监测中心,江苏常州213001 [2]污染控制与资源化研究国家重点实验室,南京大学环境学院,江苏南京210064 [3]南京工业大学环境学院,江苏南京211047
基金项目:江苏省环境监测科研基金项目(1107)
摘    要:对京杭运河常州段8个研究点位水体中的氮形态(TN、NH4+-N、NO2--N和NO3--N)和环境因子(pH、T和DO)进行了连续9个月的动态监测,全面研究了各氮形态的随时间和空间的动态变化规律,并对各氮形态及环境因子进行了相关性分析。常州段水体月平均NH4+-N变化范围为(0.589±0.351)~(3.148±1.178)mg.L-1,TN变化范围为(3.373±1.379)~(7.373±2.307)mg.L-1,枯水期到丰水期各氮形态整体表现出波动性下降趋势,其中出境断面NH4+-N下降趋势平稳,NO3--N则是主导出境断面TN含量的主要形态。各点位NH4+-N的平均浓度范围为(1.202±0.492)~(2.813±1.566)mg.L-1,TN范围为(3.520±0.504)~(8.349±3.679)mg.L-1,各形态氮含量基本呈现出上游段(S)〈新运河(G)〈老运河(L)〈下游(X)的空间分布特征,其中下游段存在一个重要的氮素上升突变段,NO3--N是对TN的贡献率(43.8%~57.4%)最大的无机态氮,其次是NH4+-N、ON、NO2--N,其中有机氮对TN的贡献率(13.3%)则以老河段最高。NH4+-N和NO3--N、TN、pH相关系数分别为0.397**、0.932**、0.261*,与DO相关系数为-0.344**,陆源输入及DO不足是京杭运河常州段氮污染严重的重要原因。

关 键 词:氮形态  时空分布  溶解氧  京杭运河

Spatio-tempo Distribution of Different Nitrogen Forms in Changzhou Segment of Grand Canal
Pan Chen,Tao Yuyan,Geng Jinju,Wang Rongjun,Chen Zhining,Han Chao,Ren Hongqiang.Spatio-tempo Distribution of Different Nitrogen Forms in Changzhou Segment of Grand Canal[J].Environmental Science and Management,2013(7):17-22.
Authors:Pan Chen  Tao Yuyan  Geng Jinju  Wang Rongjun  Chen Zhining  Han Chao  Ren Hongqiang
Institution:1.Changzhou Environmental Monitoring Center,Changzhou 213001,China;2.State Key Laboratory of Pollution Control and Resources Reuse,School of the Environment,Nanjing University,Nanjing 2l0064,China;3.School of the Environment,Nanjing University of Technology,Nanjing 211047,China)
Abstract:Different nitrogen forms(TN、NH4+-N、NO2-N,NO3-N) and environmental factors at 8 sampling sites in Changzhou Segment of the Grand Canal had been monitored for 9 months to study the spatio-tempo distribution characteristics of various nitrogen forms,as well as the correlation between different phosphorus fractions and environmental factors.Results showed that the monthly average contents of NH4+-N ranged from(0.589 ± 0.351) mg.L-1 to(3.148 ± 1.178) mg.L-1,while TN were in the range of(3.520 ± 0.504) mg.L-1 ~(7.373 ± 2.307) mg.L-1.Different nitrogen forms experienced a volatility decrease process from low flow period to high flow period,a steady decline of NH4+-N levels occurred in the river boundary section,while NO3--N might be the dominant specie affecting the TN.Spatially,the average contents of NH4+-N changed from(1.202 ± 0.492) mg.L-1 to(2.813 ± 1.566) mg.L-1,while TN varied from(3.520 ±0.504) mg.L-1 to(8.349 ± 3.679) mg.L-1.The contents of various N forms in each segment occurred in the order: downstream,(OH)3old canal,(OH)3new canal (OH)3 upstream,a sharp increase of all nitrogen forms occurred in downstream.The NO3-N form on the contribution of TN was highest(43.8% ~ 57.4%),followed by NH4+-N,ON(organic nitrogen),NO2-N,and the old canal contributed most TN of 13.3%.A significant positive correlation between NH4+-N and NO3 N,TN,pH,DO was observed with the correlation coefficients of 0.397**,0.932**,0.261* and-0.344**,terrigenous input and oxygen starvation may explain the serious nitrogen pollution in Changzhou Segment.
Keywords:different nitrogen forms  spatio-tempo distribution  dissolved oxygen  Grand Canal
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