等高反坡阶对赤水河流域上游坡耕地氮磷化学计量比与流失通量的影响

    Effects of contour reverse-slope terrace on nitrogen/phosphorus stoichiometric ratios and loss fluxes of sloping cropland in the upper reaches of Chishui River Basin

    • 摘要:
      目的 探讨布设等高反坡阶(Contour reverse-slope terrace,CRT)措施对云南赤水河流域上游坡耕地径流和氮磷流失的削减效果以及对氮磷化学计量特征和流失通量的影响。
      方法 在赤水河流域上游选取3种不同作物的坡耕地(分别种植猕猴桃、玉米、玉米间作白菜)布设CRT,以原状坡耕地为对照(CK),在2024年雨季对降雨和径流进行野外观测研究,基于8次自然降雨产流事件,分析赤水河流域上游布设CRT措施下径流各形态氮磷流失浓度、流失量、氮磷化学计量比及流失通量的变化特征。
      结果 坡耕地径流流失主要受降雨量影响,布设CRT削减55.48%的径流流失。布设CRT有效削减径流总氮(Total nitrogen,TN)、硝态氮(Nitrate nitrogen,NO3 −N)、铵态氮(Ammonium nitrogen,NH4 +−N)、总磷(Total phosphorus,TP)、正磷酸根态磷(Orthophosphate phosphorus,PO4 3−P)流失浓度及流失量,且在雨量适中阶段削减效果最为显著。赤水河流域上游坡耕地径流的氮磷化学计量比处于氮限制,CRT的氮磷化学计量比显著高于CK,表明布设CRT可有效缓解氮限制。径流是驱动各形态氮磷迁移的关键因素,CRT通过减少径流量显著降低各形态氮磷流失通量。TN流失通量是TP的2.52~5.55倍,因此在坡耕地面源污染防控中应优先关注氮素流失的管控。
      结论 CRT措施不仅显著拦截坡耕地径流及氮磷流失,还有效缓解区域径流氮限制,阻控面源污染物输出,可以显著提升坡耕地的水土保持能力。

       

      Abstract:
      Objective To investigate the effect of deploying contour reverse-slope terrace (CRT) measure on the reduction of runoff and nitrogen/phosphorus loss from sloping cropland in the upper reaches of Chishui River Basin of Yunnan Province, as well as the effect on nitrogen/phosphorus stoichiometric characteristics and flux loss.
      Method CRT were deployed on sloping cropland with three different crops (kiwifruit, corn, and corn intercropped with cabbage, respectively) in the upper reaches of Chishui River Basin, and the original sloping cropland was used as the control (CK). A field observation study of rainfall and runoff was conducted during the 2024 rainy season to analyze the change characteristics of the loss concentration, loss amount, stoichiometric ratios, and flux losses of each form of nitrogen/phosphorus in runoff under the deployment of CRT measure in the upper reaches of Chishui River Basin, based on the eight natural rainfall-produced flow events.
      Result Runoff loss of sloping cropland was mainly affected by rainfall amount, and the deployment of CRT reduced runoff loss by 55.48%. The CRT effectively intercepted and reduced the loss concentration and loss amount of runoff total nitrogen (TN), nitrate nitrogen (\mathrmNO_3^- -N), ammonium nitrogen (\mathrmNH_4^+ -N), total phosphorus (TP) and orthophosphate phosphorus (\mathrmPO_4^3- -P), with the most significant reduction effects observed during periods of moderate rainfall amount. The nitrogen/phosphorus stoichiometric ratio of runoff from sloping cropland in the upper reaches of Chishui River basin was in nitrogen limitation, while the nitrogen/phosphorus stoichiometric ratio of CRT was significantly higher than that of CK, indicating that deployment of CRT could effectively alleviate nitrogen limitation. Runoff was the key factor driving the migration of each form of nitrogen/phosphorus, and CRT significantly reduced the loss flux of nitrogen/phosphorus from each form by reducing the runoff volume. The flux loss of TN was 2.52−5.55 times that of TP, so priority attention should be given to the control of nitrogen loss in the prevention and control of surface pollution in sloping cropland.
      Conclusion CRT measure not only significantly intercepts runoff and nitrogen/phosphorus loss of sloping cropland, but also effectively alleviates nitrogen limitation in regional runoff, blocks and controls the output of surface source pollutants, and then can significantly enhance the soil and water conservation capacity of sloping cropland.

       

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