间歇性降雨条件下施肥后红壤坡耕地氮磷迁移特征

    Characteristics of Nitrogen and Phosphorus Migration in Red Soil Sloping Farmland after Fertilization under Intermittent Rainfall

    • 摘要: 为了探究间歇性降雨对施肥后的红壤坡耕地中氮磷的持续性迁出特征, 于2022年7-8月通过间歇性实施8次室内人工降雨模拟试验, 观测施肥后红壤土中地表径流和壤中流氮磷浓度及通量变化, 分析径流中不同形态氮磷的初期冲刷规律。结果表明: (1)将整个间歇性降雨试验看作一个完整的降雨周期, 氮素在壤中流中的累积流失量大于地表径流, 而磷素的流失以地表径流为主。地表径流和壤中流中氮磷的累积流失量与累积产流量之间存在显著相关关系, 可以用指数函数或对数函数对两者的关系进行拟合。(2)红壤坡耕地较易产生初期冲刷现象, 径流中各污染物发生初期冲刷的强度依次为: 溶解态磷(TDP)>总磷(TP)>颗粒态磷(TPP)>氨氮(NH4+-N)>总氮(TN)>硝态氮(NO3--N)。(3)NH4+-N、TP、TDP和TPP的迁出主要集中在前3次降雨, 且地表径流中的浓度始终大于壤中流, 壤中流发生初期冲刷的强度略高于地表径流。NO3--N和TN随径流的迁移呈现前期地表径流浓度高而后期壤中流浓度高、地表径流初期冲刷现象更为显著的特点。上述结果表明, 控制施肥后前几场降雨产流中的氮磷流失及壤中流氮的长期持续流失, 是防控华南地区红壤坡耕地面源污染的有效途径。

       

      Abstract: In order to explore the sustained migration characteristics of nitrogen and phosphorus in fertilized red soil slope farmland under intermittent rainfall, eight events of indoor artificial rainfall simulation experiments were conducted intermittently from July to August 2022 to observe the changes in concentration and flux of nitrogen and phosphorus, and to analyze the first flush effect (FFE) of different forms of nitrogen and phosphorus in runoff. The results show that: (1) If the whole intermittent rainfall experiment is regarded as a complete rainfall cycle, the cumulative loss of nitrogen in interflow is greater than that in surface runoff, while the loss of phosphorus is mainly due to surface runoff. There is a significant correlation between the cumulative loss of nitrogen and phosphorus from surface runoff and interflow. The exponential or logarithmic function can be used to fit the relationship between the cumulative nitrogen/phosphorus loss and the cumulative production flow. (2) Under the condition of intermittent rainfall, the first flush phenomenon of nitrogen and phosphorus in fertilized red soil slope farmland occurred. The intensity of FFE varied as TDP>TP>TPP>NH4+-N>TN>NO3--N. (3) The emigration of NH4+-N, TP, TDP and TPP was mainly concentrated in the first three rainfall events, and their concentrations in surface runoff were always greater than that in interflow, and their intensity of FFE in interflow was slightly higher than that in surface runoff. In contrast, the migration of NO3--N and TN with runoff exhibits a high concentration in surface runoff during early intermittent rainfall and a high concentration in interflow during later stages, and the first flush phenomenon of NO3--N and TN in surface runoff is more significant. The above results indicate that, the effective ways to prevent and control non-point source pollution of fertilized red soil slope farmland in South China are: (1) to control the loss of nitrogen and phosphorus in surface runoff and interflow in early rainfall events and (2) to pay attention to the long-term and sustained loss of nitrogen in interflow.

       

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