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 plain 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, 面临着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, 因地制宜地开展沟渠—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、半封闭和全开放3种沟浜协同治理措施下水稻生长季沟塘不同形态氮磷浓度变化, 分析氮磷迁移特征及其主要影响因素, 明晰不同沟浜协同治理措施对氮磷的去除效果。结果表明, 在时间尺度上, 整个水稻生长季, 沟塘水在施肥后第7天后铵态氮、总氮和总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, 全封闭模式对总氮和总磷的平均去除率分别为45.15%和55.40%, 且全封闭模式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; 半封闭模式下, 沟塘沿程的拦截对稻田退水中的氮磷具有很好的净化与消纳效果, 全生长季总氮和总磷的浓度呈降低趋势, 对总氮和总磷的平均去除率分别为60.28%和74.75%, 显著降低了排水接纳河流的污染风险; 开放模式对水体中总氮和总磷的平均去除率分别为22.27%和18.18%, 对氮磷的去除水平较低, 但仍具有一定去除效果。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 crisscrossed by rivers, but the slow-moving water in cut-off ditches and streams results in a weak self-purification capacity, contributing to agricultural non-point source pollution. To enhance the water purification functions of ditches and rivers in the plain river network area, it is imperative to integrate their characteristics and implement collaborative management strategies of ditches-ecological ponds-disconnected beaches-stream adaption to local conditions. In this study, we focused on the typical ditches and rivers in the Taihu Lake Basin with the aims of investigating the spatiotemporal dynamics of N and P migration, identifying the main influencing factors, and clarifying the impact of different ditch-pond management strategies on N and P removal rates. Through continuous in situ monitoring of N and P concentrations changes within ditches and ponds during the rice growth season, we assessed the effects of three modes of coordinated management of ditch-pond: fully enclosed, semi enclosed, and fully open. The results showed that, during the rice growth season, NN4+-N、TN and TP concentrations in ditch and pond water decreased and stabilized 7 days after fertilizer application, highlighting fertilizer application as the main factor influencing N and P concentrations. Spatially along the water flow pathway from rice field to the entrance of the river, the different ditch-pond coordinated management measures were the key factors influencing N and P migration. Under the three coordinated management measures for ditch-pond systmes, the average TN and TP removal rates under fully enclosed mode are 45.15% and 55.40%, respectively. Notably, the drainage from the fully enclosed ditch-pond was diverted to farmland after storage, therefore the environmental risk of pollution to surrounding water bodies was relatively small. The semi enclosed mode demonstrated excellent purification and absorption of N and P in paddy drainage. Full-growth stage, the concentrations of TN and TP showed a decreasing trend,with average removal rates of 60.28% for TN and 74.75%, respectively, considerably reducing the pollution risk to the receiving river. In contrast, the fully open mode showed lower removal rates of 22.27% for TN and 18.18% for TP, yet it still contributed to N and P removal. Overall, the coordinated management of ditch-pond for N and P interception and purification was effective in maintaining surface water quality standards and reducing the pollution risk to the surrounding environment from paddy drainage.

     

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