北京城市地表河流硝酸盐氮来源的氮氧同位素示踪研究

任玉芬, 张心昱, 王效科, 贺成武, 侯培强, 徐志伟, 欧阳志云. 北京城市地表河流硝酸盐氮来源的氮氧同位素示踪研究[J]. 环境工程学报, 2013, 7(5): 1636-1640.
引用本文: 任玉芬, 张心昱, 王效科, 贺成武, 侯培强, 徐志伟, 欧阳志云. 北京城市地表河流硝酸盐氮来源的氮氧同位素示踪研究[J]. 环境工程学报, 2013, 7(5): 1636-1640.
Ren Yufen, Zhang Xinyu, Wang Xiaoke, He Chengwu, Hou Peiqiang, Xu Zhiwei, Ouyang Zhiyun. Application of nitrogen and oxygen isotopes in study of nitrate sources in Beijing urban rivers[J]. Chinese Journal of Environmental Engineering, 2013, 7(5): 1636-1640.
Citation: Ren Yufen, Zhang Xinyu, Wang Xiaoke, He Chengwu, Hou Peiqiang, Xu Zhiwei, Ouyang Zhiyun. Application of nitrogen and oxygen isotopes in study of nitrate sources in Beijing urban rivers[J]. Chinese Journal of Environmental Engineering, 2013, 7(5): 1636-1640.

北京城市地表河流硝酸盐氮来源的氮氧同位素示踪研究

  • 基金项目:

    中国科学院知识创新工程重要方向项目 (KZCX2-EW-310)

    国家自然科学基金面上项目(41030744和40901265)

  • 中图分类号: X522

Application of nitrogen and oxygen isotopes in study of nitrate sources in Beijing urban rivers

  • Fund Project:
  • 摘要: 为了有效防治城市地表河流硝酸盐氮的污染并进行针对性水体治理,利用δ15N和δ18O双同位素示踪技术,对北京城区地表河流硝酸盐污染进行了溯源。选取北京9条河流的10个监测点,分析了硝酸盐氮污染的浓度分布特征,并运用MAT253氮氧双同位素技术解析了硝酸盐的各种来源。研究结果表明,北京城区地表河流硝酸盐氮污染自上游至下游逐渐加重,上游8个监测点的硝酸盐氮平均浓度在0.7~3.4 mg/L之间,下游东护城河和通惠河2处硝酸盐氮的浓度均值分别达7.6 mg/L和7.0 mg/L。利用同位素质谱MAT253分析,得知北京城区地表河流δ15N值总体分布范围为-1.2‰~+28.88‰,δ18O值分布范围为+0.09‰~+6.62‰,依据δ15N和δ18O的特征范围,得出北京城区地表河流硝酸盐来源主要是粪肥和污水。
  • [1] Aravena R., Evans M.L., Cherry J. A. Stable isotopes of oxygen and nitrogen in source identification of nitrate from septic systems. Ground Water, 1993, 31(2): 180-186
    [2] Amberger A., Schmidt H.L. Natürliche isotopengehalte von Nitrat als Indikatoren für dessen Herkunft. Geochimica et Cosmochimica Acta, 1987, 51(10): 2699-2705
    [3] Heaton T.H.E. Isotopic studies of nitrogen pollution in the hydrosphere and atmosphere: A review. Chemical Geology, 1986, 59(1): 87-102
    [4] Kendall C., Campbell D.H., Burns D.A., et al. Tracing sources of nitrate in snowmelt runoff using the oxygen and nitrogen isotopic compositions of nitrate. IAHS Publications-Series of Proceedings and Reports-Intern Assoc Hydrological Sciences, 1995, 228: 339-348
    [5] Wassenaar L.I. Evaluation of the origin and fate of nitrate in the Abbotsford Aquifer using the isotopes of 15N and 18O in NO3- Applied Geochemistry, 1995, 10(4): 391-405
    [6] Campbell D.H., Kendall C., Chang C.C.Y., et al. Pathways for nitrate release from an alpine watershed: Determination using δ15N and δ18O. Water Resoures Research, 2002, 38(5): 101-109
    [7] Silva S., Ging P., Lee R., et al. Forensic applications of nitrogen and oxygen isotopes in tracing nitrate sources in urban environments. Environmental Forensics, 2002, 3(2): 125-130
    [8] Ging P.B., Lee R.W.,Silva S.R. Water Chemistry of Shoal Creek and Waller Creek, Austin, Texas and Potential Sources of Nitrate. USGS Water-Resources Investigations Report, 1996
    [9] Battaglin W.A., Kendall C., Chang C.C.Y., et al. Chemical and isotopic evidence of nitrogen transformation in the Mississippi River, 1997-98. Hydrological Processes, 2001, 15(7): 1285-1300
    [10] Chang C.C.Y., Kendall C., Silva S.R., et al. Nitrate stable isotopes: Tools for determining nitrate sources among different land uses in the Mississippi River Basin. Canadian Journal of Fisheries and Aquatic Sciences, 2002, 59(12): 1874-1885
    [11] 周爱国, 蔡鹤生. 硝酸盐中δ15N 和δ18O的测试新技术及其在地下水氮污染防治研究中的进展. 地质科技情报, 2001, 20(4): 94-98 Zhou A. G., Cai H. S., Liu C. F. A new analytical technique of isotope 15N and 18O in NO and the development in N contam inative study of groundwater. Geological Science and Technology Information, 2001, 20(4): 94-98 (in Chinese)
    [12] 肖化云,刘丛强,李思亮. 贵阳地区夏季雨水硫和氮同位素地球化学特征.地球化学,2003,32(3):248-254 Xiao H.Y, Liu C.Q., Li S.L. Geochemical characteristics of sulfur and nitrogen isotopic compositions in rains of Guiyang in summer. Geochimica, 2003, 32(3): 248-254(in Chinese)
    [13] 陈法锦, 李学辉, 贾国东. 氮氧同位素在河流硝酸盐研究中的应用. 地球科学进展, 2007, 22(12):1251-1257 Chen F. J., Li X. H., Jia G. D. The application of nitrogen and oxygen isotopes in the study of nitrate in rivers. Advances in Earth Science, 2007, 22(12):1251-1257 (in Chinese)
    [14] Xue D., Botte J., De Baets B., et al. Present limitations and future prospects of stable isotope methods for nitrate source identification in surface-and groundwater. Water Research, 2009, 43(5): 1159-1170
    [15] Fukada T., Hiscock K.M., Dennis P.F., et al. A dual isotope approach to identify denitrification in groundwater at a river-bank infiltration site. Water Research, 2003, 37(13): 3070-3078
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  • 收稿日期:  2012-02-08
  • 刊出日期:  2013-05-22
任玉芬, 张心昱, 王效科, 贺成武, 侯培强, 徐志伟, 欧阳志云. 北京城市地表河流硝酸盐氮来源的氮氧同位素示踪研究[J]. 环境工程学报, 2013, 7(5): 1636-1640.
引用本文: 任玉芬, 张心昱, 王效科, 贺成武, 侯培强, 徐志伟, 欧阳志云. 北京城市地表河流硝酸盐氮来源的氮氧同位素示踪研究[J]. 环境工程学报, 2013, 7(5): 1636-1640.
Ren Yufen, Zhang Xinyu, Wang Xiaoke, He Chengwu, Hou Peiqiang, Xu Zhiwei, Ouyang Zhiyun. Application of nitrogen and oxygen isotopes in study of nitrate sources in Beijing urban rivers[J]. Chinese Journal of Environmental Engineering, 2013, 7(5): 1636-1640.
Citation: Ren Yufen, Zhang Xinyu, Wang Xiaoke, He Chengwu, Hou Peiqiang, Xu Zhiwei, Ouyang Zhiyun. Application of nitrogen and oxygen isotopes in study of nitrate sources in Beijing urban rivers[J]. Chinese Journal of Environmental Engineering, 2013, 7(5): 1636-1640.

北京城市地表河流硝酸盐氮来源的氮氧同位素示踪研究

  • 1.  中国科学院生态环境研究中心城市与区域生态国家重点实验室,北京 100085
  • 2.  中国科学院地理科学与资源研究所生态系统网络观测与模拟重点实验室,北京 100101
  • 3.  河南理工大学资源环境学院,焦作 454003
基金项目:

中国科学院知识创新工程重要方向项目 (KZCX2-EW-310)

国家自然科学基金面上项目(41030744和40901265)

摘要: 为了有效防治城市地表河流硝酸盐氮的污染并进行针对性水体治理,利用δ15N和δ18O双同位素示踪技术,对北京城区地表河流硝酸盐污染进行了溯源。选取北京9条河流的10个监测点,分析了硝酸盐氮污染的浓度分布特征,并运用MAT253氮氧双同位素技术解析了硝酸盐的各种来源。研究结果表明,北京城区地表河流硝酸盐氮污染自上游至下游逐渐加重,上游8个监测点的硝酸盐氮平均浓度在0.7~3.4 mg/L之间,下游东护城河和通惠河2处硝酸盐氮的浓度均值分别达7.6 mg/L和7.0 mg/L。利用同位素质谱MAT253分析,得知北京城区地表河流δ15N值总体分布范围为-1.2‰~+28.88‰,δ18O值分布范围为+0.09‰~+6.62‰,依据δ15N和δ18O的特征范围,得出北京城区地表河流硝酸盐来源主要是粪肥和污水。

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