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当前位置: 首页 > 文章 > 模拟降雨条件下坡度对茶园红壤氮素流失影响 农业环境科学学报 2014,33 (05) 178-184
Position: Home > Articles > Impacts of Slope on Nitrogen Losses from Red Soil in Tea Garden Under Simulated Rainfall Journal of Agro-Environment Science 2014,33 (05) 178-184

模拟降雨条件下坡度对茶园红壤氮素流失影响

作  者：
赵越;李泽利;刘茂辉;钱丽萍;孙云;王振;王玉秋
单  位：
黄山学院生命与环境科学学院;南开大学环境科学与工程学院;环境保护部环境规划院
关键词：
新安江;茶园红壤;坡度;模拟降雨;氮素;流失特征
摘  要：
以新安江流域茶园红壤为研究对象,采用人工模拟降雨方法,研究其在五种不同坡度(0°、5°、10°、15°、20°)下的产流和氮素流失的特征。结果显示,径流以壤中流为主,地表径流中的氮素在流失过程中表现出了很强的初期冲刷效应,壤中流的氮素流失量随着降雨的持续而逐渐增大;在各种坡度下,氮素均以壤中流流失为主;地表径流中总氮、硝态氮、氨氮的流失量y与坡度x的回归方程分别为y=1.03e0.06x-0.88(R2=0.99**)、y=0.37e0.06x-0.36(R2=0.98**)、y=0.002x+0.004(R2=0.94**),壤中流中总氮、硝态氮、氨氮的流失量y与坡度x的回归方程分别为y=-5.65e0.06x+30.49(R2=0.91**)、y=-0.17e0.16x+14.92(R2=0.98*)、y=0.77e-0.18x+0.13(R2=0.92*)。随着坡度的增大,地表径流中氮素的流失呈增大趋势,壤中流中氮素的流失呈下降趋势。
译  名：
Impacts of Slope on Nitrogen Losses from Red Soil in Tea Garden Under Simulated Rainfall
作  者：
ZHAO Yue;LI Ze-li;LIU Mao-hui;QIAN Li-ping;SUN Yun;WANG Zhen;WANG Yu-qiu;Chinese Academy for Environment Planning;College of Environmental Science and Engineering,Nankai University;College of Biology and Environmental Science,Huangshan University;
关键词：
Xin′anjiang River;;red soil in tea garden;;slope;;simulated rainfall;;nitrogen;;losses
摘  要：
Slope plays important roles in nutrient losses from soils, especially under rainfall. A laboratory simulated rainfall experiment was conducted to investigate the characteristics of runoff and nitrogen losses from red soil in tea garden in Xin′anjiang River Basin under five slope gradients of 0°, 5°, 10°, 15° and 20°. Results showed that runoff occurred mainly as interflow. Nitrogen losses in surface runoff had initial flush effect after each raining event, whereas those in the interflow increased with raining time. Under all slope gradients, nitrogen losses were mainly through interflow. For the surface runoff, regression equation for nitrogen losses(y)and slopes(x)was y=1.03e0.06x-0.88 with R2=0.99** for total nitrogen, y=0.37e0.06x-0.36 with R2=0.98** for NO-3-N, and y=0.002x+0.004 with R2=0.94** for NH+ 4-N. For the interflow, that was y=-5.65e0.06x+30.49 with R2=0.91** for total N, y=-0.17e0.16x+14.92 with R2=0.98* for NO-3-N, and y=0.77e-0.18x+0.13 with R2= 0.92* for NH+ 4-N. These equations indicated that with increasing slopes nitrogen losses increased in the surface runoff, but decreased in the interflow.

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