中国地质大学(武汉)环境学院
纸质出版:2025
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周志浩, 罗明明, 陈静, 等. 集中补给条件对岩溶地下河水文过程及污染响应的影响[J]. 地质科技通报, 2025,44(3):324-333.
周志浩, 罗明明, 陈静, et al. 集中补给条件对岩溶地下河水文过程及污染响应的影响[J]. Bulletin of Geological Science and Technology, 2025, 44(3): 324-333.
周志浩, 罗明明, 陈静, 等. 集中补给条件对岩溶地下河水文过程及污染响应的影响[J]. 地质科技通报, 2025,44(3):324-333. DOI: 10.19509/j.cnki.dzkq.tb20230566.
周志浩, 罗明明, 陈静, et al. 集中补给条件对岩溶地下河水文过程及污染响应的影响[J]. Bulletin of Geological Science and Technology, 2025, 44(3): 324-333. DOI: 10.19509/j.cnki.dzkq.tb20230566.
集中补给条件往往对岩溶地下河的水量和水质有显著影响,因此明晰不同集中补给条件对其的影响具有重要意义。基于水文地球化学调查,对鄂西青龙口地下河系统的落水洞入口和地下河出口同步进行了水文和水化学动态监测,探讨了不同补给条件对地下河水量和水质的影响。结果表明:补给强度和土壤含水率直接控制着落水洞的产汇流过程及岩溶地下河的流量响应,未达到阈值的降雨事件不会引起地下河流量响应;降雨集中汇流至落水洞入口的过程中,各水化学离子浓度均有明显的提高,而青龙口地下河出口水化学响应受补给强度影响,强降雨下地下河受落水洞入口水化学离子浓度富集影响强烈;降雨后的水质波动主要源于降雨形成地表径流携带的面源污染,暴雨后的总无机氮和磷酸盐在落水洞口出现聚集,集中补给输入的污染物对地下河产生直接污染,浓度可达天然背景值的2~3倍;水化学响应中氨氮先于硝态氮进入岩溶水循环,地下河系统出口的硝态氮和总无机氮通量相较入口有所增加,氨氮通量随补给时间逐渐减少,推测管道内发生了硝化反应。本研究结果可为岩溶地下河的污染防控和水环境治理提供科学依据。
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