Characteristics of runoff processes and nitrogen loss via surface flow and interflow from weathered granite slopes of Southeast China Characteristics of runoff processes and nitrogen loss via surface flow and interflow from weathered granite slopes of Southeast China

最小化 最大化

Vol16 No.5: 1048-1064

Title】Characteristics of runoff processes and nitrogen loss via surface flow and interflow from weathered granite slopes of Southeast China

Author】DENG Long-zhou 1,2; FEI Kai 1,2; SUN Tian-yu 1,2; ZHANG Li-ping 1,2*; FAN Xiao-juan 1,2 ; NI Liang 3

Addresses】1 College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China; 2 Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Hangzhou 310058, China; 3 Agricultural Experiment Station, Zhejiang University, Hangzhou 310058, China

Corresponding author】ZHANG Li-ping

Citation】Deng LZ, Fei K, Sun TY, et al. (2019) Characteristics of runoff processes and nitrogen loss via surface flow and interflow from weathered granite slopes of Southeast China. Journal of Mountain Science 16(5). https://doi.org/10.1007/s11629-018-5253-2

DOI】https://doi.org/10.1007/s11629-018-5253-2

Abstract】Rainfall intensity and slope gradient are two of the most important factors affecting the variations of runoff nitrogen (N). However, the effects of slope gradient and rainfall intensity on N loss via surface flow and interflow onweathered granite slopes are poorly understood. In this study, 12 artificial rainfalls (three rainfall intensities and four slope gradients) were simulated to investigate the coupling loss characteristics of surface flow–interflow–total nitrogen (TN), nitrate nitrogen (NO3-N) and ammonia nitrogen (NH4+-N) on weathered granite slopes. The results show that slope gradient has a greater impact on the surface flow when the rainfall intensity is relatively large. The effect gradually weakens with the decrement of rainfall intensity. The interflow yield increases firstly with the prolongation of rainfall duration, then tends to be stable and finally decreases. The total surface flow percentage increases with rainfall intensity while it decreases with increasing slope gradient with a range of 10.88%-71.47%. The TN loss concentration of the surface flow continually decreases with rainfall duration while that of the interflow shows different fluctuations. However, the TN loss loads of both surface flow and interflow increase with increasing rainfall intensity and slope gradient. The NO3-N concentration of interflow is much higher than that of the surface flow. The NH4+-N concentration is always less than that of NO3-N with no significant difference between surface flow and interflow. The percentages of the TN, NO3-N, and NH4+-N total loss load and concentration of surface flow and interflow were analyzed. The results show that N loss via both surface flow and interflow occurs mainly in the form of NO3-N. Most of the N loss is caused by interflow which is the preferential path of runoff nutrient loss. These findings provide data support and underlying insights for the control of runoff and N loss on the weathered granite slopes.

Keywords】Simulated rainfall; Nitrogen loss; Surface flow; Interflow; Slope gradient; Rainfall intensity; Weathered granite slope