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    郭高轩, 代垠东, 许亮, 朱琳, 戚琦, 欧志亮, 沈媛媛. 北京市岩溶地下水质量评价及其生态环境效应[J]. 中国地质. DOI: 10.12029/gc20230423001
    引用本文: 郭高轩, 代垠东, 许亮, 朱琳, 戚琦, 欧志亮, 沈媛媛. 北京市岩溶地下水质量评价及其生态环境效应[J]. 中国地质. DOI: 10.12029/gc20230423001
    GUO Gaoxuan, DAI Yindong, XU Liang, ZHU Lin, QI Qi, OUZhiliang, SHEN Yuanyuan. Evaluation of karst groundwater quality in Beijingand its eco-environmental effects[J]. GEOLOGY IN CHINA. DOI: 10.12029/gc20230423001
    Citation: GUO Gaoxuan, DAI Yindong, XU Liang, ZHU Lin, QI Qi, OUZhiliang, SHEN Yuanyuan. Evaluation of karst groundwater quality in Beijingand its eco-environmental effects[J]. GEOLOGY IN CHINA. DOI: 10.12029/gc20230423001

    北京市岩溶地下水质量评价及其生态环境效应

    Evaluation of karst groundwater quality in Beijingand its eco-environmental effects

    • 摘要:研究目的】岩溶地下水是北京市重要的供水水源,在城市供水安全保障中发挥着难以替代的作用,同时又具有重要的生态功能。【研究方法】本文通过对2021年6月在北京市内系统采集的278件岩溶地下水样化验数据为基础,以岩溶水系统为单元,开展了岩溶水单因子质量评价和多因子综合评价,并首次对有机指标进行了统计和分析。【研究结果】(1)北京市岩溶水的pH、TDS和TH分别为7.69、334.77mg·L-1和262.01mg·L-1,具有弱碱性、低盐度和低硬度的特点,地下水质量总体良好。(2)非常规指标的检出率从大到小为:苯并a芘(4.32%)、三溴甲烷(3.60%)和二甲苯(总量)(2.52%),分布较分散,应当引起足够重视。(3)北京市岩溶水水质Ⅰ-Ⅲ类总占比为82.01%,Ⅳ和Ⅴ类总占比为17.99%,超标点主要集中在山区与平原分界线处。各系统超标率大小为大兴-通州(75.00%) >北务(60.00%) >昌平(18.18%) >西山(16.94%) >顺平(16.00%)>千家店-九渡河(15.56%)>延庆(11.76%),其中影响北京市地下水质量的指标主要有Fe、TH、NH3-N、Mn、SO42-、F-、NO3-N等。(4)应通过提高植被覆盖率加强水源涵养以增加补给量,应严格控制点源和面源污染减少污染物输入,持续优化监测网络进行预警,广泛宣传增强公众生态环保意识,共同保护岩溶水的生态环境。

       

      Abstract: Objective As an important water supply source in Beijing, Karst groundwater played an irreplaceable role in the security of urban water supply and ecological environment improvement in Beijing city. Methods Based on the laboratory data of 278 karst groundwater samples collected systematically in Beijing karst water system in June 2021, the single factor quality evaluation and multi-factor comprehensive evaluation of karst water were carried out with karst water system as the unit, and the organic indexes were counted and analyzed for the first time. Results (1) The medians of pH, TDS and TH concentration of karst water in Beijing are 7.69, 334.77 mg·L-1 and 262.01 mg·L-1 respectively, which are characterized by weak alkalinity, low salinity and low hardness. The concentration of TH, TDS, SO42- and Cl- in Daxing-Tongzhou karst water system and Xishan karst water system are significantly higher than those in other karst water systems. (2) From large to small, the detection rate of unconventional indicators is:benzopyrene (4.32%) > tribromomethane (3.60%) > xylene (totalamount) (2.52%).The distribution of organic matter detection is relatively scattered and should be given sufficient attention.(3) The results of groundwater quality evaluation show that the total proportion of class I-III karst water quality in Beijing is 82.01%, with an exceeding rate of 17.99%. The exceeding points are mainly concentrated at the boundary between mountainous areas and plain area.The overstandard rate of each system was Daxing-Tongzhou (75.00%) > Beiwu (60.00%) > Changping (18.18%) >Xishan (16.94%) >Shunping (16.00%) >Qianjiadian-Jiuduhe (15.56%) > Yanqing (11.76%). Among them, Fe, TH, NH3-N, Mn, SO42-, F- andNO3-N are the main indexes affecting groundwater quality in Beijing. (4) In order to protect andimprovethe karst water ecological environment practically, methods such as strengthening water conservation to increase recharge, control point source and non-point source pollution to reduce pollutant input, continue monitoring and give play to early warning, and widely publicize and enhance public awareness should be appliedsystematically in the future.

       

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