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永定河冲洪积扇地下水中硝酸盐来源的同位素识别
Identification of nitrate sources in groundwater in the Yongding River alluvial fan with isotope technology
【摘要】 硝酸盐(NO3-)是北京地下水的主要污染物之一。本文分析了永定河冲积扇不同部位第四系地下水的水化学和氮、氧同位素特征,识别了地下水中NO3-的主要污染源,并定量评价了各种源的贡献。研究区地下水的NO3--N浓度介于1.3237.44 mg/L,80%的地下水样NO3--N浓度超过我国《生活饮用水卫生标准》(20 mg/L)。地下水的δ15N-NO3-值介于+9.38‰+16.96‰,均值12.87‰,δ18O-NO3-值介于+3.13‰+21.18‰,均值+10.39‰,结合反硝化作用的识别,推断地下水中NO3-主要来自粪肥,部分来自NO3-化肥和大气降水。采用氮、氧同位素和物质平衡混合模型定量评价表明,粪肥对地下水NO3-的贡献为58%81%,据此提出了保护和改善地下水水质的建议。
【Abstract】 Nitrate(NO3-) is one of the main contaminants in groundwater in Beijing. In this study,thecharacteristics of hydrochemistry, nitrogen isotope(15N- NO3-) and oxygen isotope(18O- NO3-) in differentparts of the quaternary groundwater are analyzed in the Yongding River alluvial fan. The contaminant sourc-es of NO3-in the groundwater are identified,and the contributions of these different contaminant sources tothe NO3-are evaluated quantitatively. The concentrations of NO3--N in the groundwater range from 1.32 mg/L to 37.44 mg/L,The concentrations of NO3--N in 80% of the groundwater samples exceeded the drinkingwater standarnd of 20 mg/L. The values of15N-NO3-in groundwater range from +9.38‰ to +16.96‰ andthe mean value is +12.87‰. The values of18O-NO3-in groundwater range from +3.13‰ to +21.18‰ andthe mean value is +10.39‰. Combined with the identification of denitrification in groundwater,NO3-mainlycome from manure and partly come from chemical fertilizer and precipitation. Quantitative evaluation withisotope techniques and material balance model shows that manure contributes 58%81% to the concentra-tion of NO3-in groundwater. On the basis of this study,the suggestion about how to protect and improvegroundwater quality is recommended.
【Key words】 groundwater; nitrate; isotope technique; contaminant source;
- 【文献出处】 水利学报 ,Journal of Hydraulic Engineering , 编辑部邮箱 ,2016年04期
- 【分类号】X523
- 【被引频次】18
- 【下载频次】494