Effect of microrelief features of tillage methods under different rainfall intensities on runoff and soil erosion in slopes

被引:12
|
作者
Zhao, Xinkai [1 ]
Song, Xiaoyu [1 ]
Li, Lanjun [1 ]
Wang, Danyang [2 ]
Meng, Pengfei [1 ]
Li, Huaiyou [3 ]
机构
[1] Xian Univ Technol, State Key Lab Ecohydraul Northwest Arid Reg, Xian 710048, Shaanxi, Peoples R China
[2] Beijing Guanting Reservoir Management Off, Zhangjiakou 075441, Peoples R China
[3] Yellow River Conservancy Comm, Xifeng Expt Stn Soil & Water Conservat, Qingyang 745000, Gansu, Peoples R China
基金
中国国家自然科学基金;
关键词
Simulated rainfall; Tillage methods; Microrelief features; Runoff; Soil erosion; SURFACE-ROUGHNESS; LOESS PLATEAU; OVERLAND-FLOW; DEPRESSION-STORAGE; INTERRILL EROSION; WATER EROSION; C-FACTOR; INFILTRATION; RUSLE; VARIABILITY;
D O I
10.1016/j.iswcr.2023.10.001
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Tillage methods play a crucial role in controlling rainwater partitioning and soil erosion. This study utilized rainfall simulation experiments to investigate the impact of four tillage methods (manual digging (MD), manual hoeing (MH), traditional ploughing (TP), and ridged ploughing (RP)) on runoff and soil erosion at the plot scale. The smooth slope (SS) was used as a benchmark. Rainfall intensities of 30, 60, 90, and 120 mm h(-1) were considered. The study revealed that tillage altered rainwater distribution into depression storage, infiltration, and runoff. Tillage reduces runoff and increases infiltration. The four tillage methods (30-73%) increased the proportion of rainwater converted to infiltration to varying degrees compared to the SS (22-53%). Microrelief features influenced the role of tillage methods in soil erosion. Surface roughness and depression storage accounted for 79% of the variation in sediment yield. The four tillage methods reduced runoff by 2.1-64.7% and sediment yield by 2.5-77.2%. Moreover, increased rainfall intensity weakens the ability of tillage to control soil erosion. When rainfall intensity increased to 120 mm h(-1), there was no significant difference in runoff yield among RP, TP, MH, and SS. Therefore, assessing the effectiveness of tillage in reducing soil erosion should consider changes in rainfall intensity. Additionally, the cover management (C) factor of the RUSLE was used to assess the effects of different tillage methods on soil loss. Overall, the C factor values for tilled slopes are in the order MH > TP > RP > MD with a range of 0.23-0.97. As the surface roughness increases, the C factor tends to decrease, and the two are exponential functions (R-2 = 0.86). These studies contribute to our understanding of how different tillage methods impact runoff and soil erosion in sloped farmland and provide guidance for selecting appropriate local manual tillage methods. (c) 2023 International Research and Training Center on Erosion and Sedimentation, China Water and Power Press, and China Institute of Water Resources and Hydropower Research. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BYNC -ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
引用
收藏
页码:351 / 364
页数:14
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