WANG Qi, GUO Xueru, DUAN Xiaogang, WANG Shufang, ZUO Rui, WANG Jinsheng, LIU Xin, ZHAI Yuanzheng, MENG Li. Identification and correlation of sensitive indicators for groundwater quality in South water recharge areas[J]. Journal of Beijing Normal University(Natural Science), 2023, 59(2): 288-298. DOI: 10.12202/j.0476-0301.2022313
Citation: WANG Qi, GUO Xueru, DUAN Xiaogang, WANG Shufang, ZUO Rui, WANG Jinsheng, LIU Xin, ZHAI Yuanzheng, MENG Li. Identification and correlation of sensitive indicators for groundwater quality in South water recharge areas[J]. Journal of Beijing Normal University(Natural Science), 2023, 59(2): 288-298. DOI: 10.12202/j.0476-0301.2022313

Identification and correlation of sensitive indicators for groundwater quality in South water recharge areas

  • Groundwater level and water quality data in Tongzhou District, Beijing from 2011-2019 were used to construct ROC curves of some water quality indicators before and after recharge of South-to-North water in the area.The following were identified: highly sensitive indicator Fe3+ with AUC value > 0.7, moderately sensitive indicators \rmNO_3^- , \rmNO_2^- and F with AUC values between 0.6~0.7. Concentration of Fe3+ was found to have become lower after recharge, but concentrations of \rmNO_3^- , \rmNO_2^- and F increased. A R-V copula model was constructed taking index F as an example.Indicators closely related to the sensitivity of F were found to be Ca2+, Mg2+, Na+, Cl, pH.Ca2+ and Fwere found markedly negatively correlated.After groundwater recharge, area Ca2+ concentration was found to have decreased, which stimulated Factivity; pH and F showed an indirect correlation via Ca2+.With increased pH and alkaline environment, water Ca2+ activity decreased, this was beneficial for F enrichment.Fshowed positive correlations with Mg2+, Na+, Cl.The correlation between Mg2+ and F was due to the lixiviation and intimate hydraulic connection.Simultaneous increases in Cl and F were due to displacement reaction.When Ca2+ concentration was low, Na+ would adsorb and desorb with F, F could therefore be enriched.The sensitive enrichment of F in groundwater after recharge was due to 2 reasons. On the one hand, recharge stimulated dissolution of fluorine-containing minerals of primary geological origin and mixed dilution to promote dissolution of fluorine-containing minerals. On the other hand, recharge accelerated the mutual displacement of Cl and F, plus adsorption and desorption of Na+ and Cl.The present work helps deepen the understanding of the evolution mechanism of groundwater quality in South-to-North water recharge area, also provides theoretical support and decision-making basis regarding groundwater monitoring, managing and water supply security in Beijing municipal administrative center.
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