北京张坊应急备用水源地水位动态多时间尺度演变特征及安全供水调控

    Multi-temporal scale characteristics of groundwater level dynamics and safe water supply regulation at Zhangfang emergency backup water source in Beijing

    • 摘要:
      研究目的 本文旨在明晰地下水位驱动力,实现安全供水定量调控,以保障地下水动态均衡管理、提高水资源战略储备能力。
      研究方法 依托张坊特大型傍河岩溶水源地多年逐月逐日地下水位埋深动态监测资料,采用逐步回归分析方法定量确定多时间尺度下水源地地下水位埋深动态的驱动影响因素,并利用回归模型进行供水安全调控预测。
      研究结果 月尺度下,水位埋深受前1月降水量影响最显著,其次是当月开采量、前1月水位埋深、前2月降水量;日尺度下,水位埋深受当日张坊站流量影响最显著,其次是当日降水量、当日开采量、前1日开采量、前1日水位埋深。
      结论 不同时间尺度下,自然因素是导致地下水位埋深动态变化的直接驱动因素。结合水源地含水层特征,地下水埋深对当日地表水和降水产生迅速响应,得益于表层岩溶裂隙带来的“地表−地下”紧密水力联系;而对前1~2月降水的滞后响应,表明地下水补给来源于深远部岩溶裂隙水流。供水安全调控预测结果显示,在开采极限水位埋深60 m、连续3年枯水年约束条件下,枯水期4—7月可适当加大开采,极限开采量为810×104 m3/月。

       

      Abstract:
      Objective Clarifying the driving forces of groundwater level and achieving quantitative control of water supply are crucial ways to ensure dynamic balanced management of groundwater and enhance the strategic reserve capacity of water resources.
      Methods Based on the daily and monthly monitoring data of groundwater depth over the years at the Zhangfang large karstic groundwater source area adjacent to a river, this paper employs stepwise regression analysis to quantitatively determine the driving factors influencing the dynamics of groundwater depth at the water source across multiple time scales. The regression model is then used for predictive control of water supply safety.
      Results On a monthly scale, the most significant factor influencing groundwater depth is the precipitation from the previous month, followed by the current month's extraction volume, the depth from the previous month, and precipitation from two months ago. On a daily scale, the most significant factor is the current day's flow at the Zhangfang station, followed by the current day's precipitation, the current day's extraction volume, the previous day's extraction volume and the depth from the previous day.
      Conclusions Across different time scales, natural factors is the direct driving factor causing dynamic changes in groundwater depth. Combining the aquifer characteristics of the water source, the groundwater depth responds rapidly to surface water and precipitation on the same day, benefiting from the close hydraulic connection between the surface and groundwater facilitated by surface karst fissures. The delayed response to precipitation from one to two months ago indicates that groundwater recharge originates from water flow in deep karst fissures. The results of the water supply safety regulation prediction show under the conditions of a maximum allowable groundwater depth of 60 meters and three consecutive years of low−water periods, extraction can be appropriately increased during the dry season from April to July, with the maximum extraction volume of 810×104 m3/month.

       

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