平原河网区沟浜协同措施下氮磷时空迁移特征

Characteristics of spatial and temporal transport of N and P under coordinated management of ditches and rivers in the plains river network area

  • 摘要: 我国南方平原河网区河道纵横, 但断头浜与小河道水流平缓、自净能力弱, 面临农业面源污染的严峻挑战。为提升平原河网区沟渠水质净化功能, 需要结合沟浜特点, 因地制宜开展沟渠-池塘-断头浜-小河协同治理。本文以太湖流域典型沟浜为研究对象, 聚焦氮磷迁移问题, 通过连续原位监测全封闭、半封闭、全开放3种沟浜协同治理措施下水稻生长季沟塘氮磷不同形态浓度变化, 分析了氮磷的时空动态迁移特征和主要影响因素, 明晰了不同沟浜协同治理措施对氮磷的去除率效果。结果表明, 在时间尺度上, 整个水稻生长季, 沟塘水在施肥第7天后氮磷浓度降低并趋于稳定状态, 施肥是影响沟塘氮磷浓度变化的主要因素; 在水质空间沿程路径上, 不同沟浜协同治理措施是影响氮磷迁移的关键因素。3种沟浜协同治理措施下, 总氮和总磷的浓度沿程均降低, 全封闭模式沟塘对总氮、总磷的平均去除率为45.15%、55.40%, 且全封闭模式沟塘排水贮存后循环进入农田, 因此对周围水体污染的环境风险较小; 半封闭经过沟塘沿程的拦截对稻田退水中的氮磷有很好的净化与消纳, 对总氮、总磷的平均去除率为60.28%、74.75%, 显著降低了对排水接纳河流的污染风险; 开放模式对水体中的总氮、总磷的平均去除率分别为22.27%、18.18%, 对氮磷的去除水平较低但仍有一定去除效果。沟浜协同治理对氮磷均具有一定拦截净化效果, 有效保障了地表水水质功能达标, 减轻了稻田退水对周围受纳水体环境的污染风险。

     

    Abstract: The river network area of the southern plains of China is criss-crossed by rivers, but the slow-moving water in cut-off channels and small rivers results in weak self-purification capacity, posing a serious challenge from agricultural surface pollution. To enhance the water purification function of ditches and beaches in the plains river network area, it is imperative to integrate their characteristics and implementc ollaborative management strategies tailored to local conditions, encompassing ditches, ecological ponds, disconnected beaches, and small rivers. This paper focuses on the typical ditches and beaches of Taihu Lake Basin, specifically addressing the issue of nitrogen and phosphorus migration. Through continuous in-situ monitoring of nitrogen and phosphorus concentration changes in different forms within ditches and ponds during the rice growing season, the study assesses the effects of three synergistic management measures for ditches and banks: fully enclosed, semi-enclosed, and fully open. The analysis delves into the spatiotemporal dynamics of nitrogen and phosphorus migration characteristics, identifies the main influencing factors, and clarifies the impact of the different ditch and bank management stratigies on nitrogen and phosphorus removal rates The results showed that, on the time scale over the rice growing season, nitrogen and phosphorus concentrations in ditch pond water decreased and stabilised after the 7d of fertiliser application, highlighting fertiliser application as the main factor influencing these concentrations, Spatially along the water flow pathway from rice field to the entrance of rive, the different ditch-bank synergistic management measures were the key factors influencing the nitrogen and phosphorus migration. Under the three different ditch-bank synergistic management measures emerge as key factors influencing nitrogen and phosphorus migration. Under the three management strategies, TN and TP concentrationsdecreased along the course of the ditch. In the fully closed mode, the average removal rates for TN and TP were 45.15% and 55.40%, respectively. Notably, the drainage water from the fully closed mode ditch pond was recycled into farmland after storage, minimizing the environmental risk of polluting surrounding water bodies.The semi-closed type demonstrates excellent purification and absorption of nitrogen and phosphorus in paddy retreat water, with average removal rates of 60.28% for TN and 74.75% for TP, significantly reducing the pollution risk to the receiving river. In contrast, the open-type model shows lower removal rates of 22.27% and 18.18%, yet still contributes to nitrogen and phosphorus removal.Overall, the synergistic management of ditches and banks for nitrogen and phosphorus interception and purification proves effective in maintaining surface water quality standards and reducing the risk of paddy field pollution to the surrounding environment.Overall, the synergistic management of ditches and banks for nitrogen and phosphorus interception and purification proves effective in maintaining surface water quality standards and reducing the risk of paddy field pollution to the surrounding environment.

     

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