长江科学院院报 ›› 2019, Vol. 36 ›› Issue (1): 41-47.DOI: 10.11988/ckyyb.20170619

• 水土保持与生态建设 • 上一篇    下一篇

雨强和地表糙度对坡面微地形及侵蚀的影响

李清溪, 丁文峰, 朱秀迪, 庞延杰   

  1. 长江科学院 水土保持研究所, 武汉 430010
  • 收稿日期:2017-06-27 出版日期:2019-01-01 发布日期:2019-01-17
  • 通讯作者: 丁文峰(1975-),男,教授级高级工程师,博士,研究方向为土壤侵蚀与水土保持。E-mail:wenfengding@163.com
  • 作者简介:李清溪(1992-),男,湖北京山人,硕士研究生,主要从事水土保持研究。E-mail:leeqingxi@126.com
  • 基金资助:
    国家自然科学基金项目(41271303,40901135);“十一五”科技支撑计划课题(2008BAD98B02)

Effects of Rainfall Intensity and Land Surface Roughness on Microtopography and Runoff and Sediment Yield of Slope

LI Qing-xi, DING Wen-feng, ZHU Xiu-di, PANG Yan-jie   

  1. Department of Soil and Water Conservation Research, Yangtze River ScientificResearch Institute, Wuhan 430010, China
  • Received:2017-06-27 Online:2019-01-01 Published:2019-01-17

摘要: 地表糙度是影响坡面侵蚀产沙的重要因素之一,以往研究多关注糙度对坡面产流产沙特征的影响,而较少关注不同糙度条件下坡面微地形变化和侵蚀产沙的关系。通过人工模拟降雨试验,结合Photoscan技术研究了不同雨强和地表糙度对坡面微地形及产流产沙的影响。结果表明:在试验条件下,降雨后光滑坡面和粗糙坡面4个微地形因子(地表糙度、地形起伏度、地表切割度、洼地蓄积量)数值均减小,且有随雨强增大,其减幅增大的趋势;相同雨强和降雨历时条件下,粗糙坡面微地形因子变化幅度大于光滑坡面,微地形因子变化量与侵蚀产沙量呈明显正相关;与光滑地表相比,粗糙地表只在降雨初期能有效减少产流,随着降雨时间延长,2种坡面的产流率趋于一致;在试验选取的4个雨强条件下,粗糙坡面和光滑坡面产流率均呈现先增大后趋于稳定的趋势。粗糙坡面产沙率和产流率变化规律一致,但光滑坡面产沙率表现出在产流初期迅速增大,而后呈降低并趋于稳定的趋势。研究结果可为揭示坡面土壤侵蚀机理和建立坡面侵蚀产沙模型提供参考。

关键词: 雨强, 地表糙度, 微地形, 产流, 产沙

Abstract: Surface roughness is an important factor affecting sediment yield. Previous studies are focused on the effect of roughness on runoff and sediment characteristics rather than the relationship between microtopography changes and soil erosion and sediment yield process under different roughness conditions. In this study, the effects of rainfall intensity and land surface roughness on microtopography and runoff and sediment yield are studied by artificial rainfall experiments and Photoscan technique. Results reveal that in the experiment condition, four microtopographic factors, inclusive of surface roughness, relief amplitude, surface incision, and depression storage) decrease on both smooth and rough slopes after rainfall, and the decreasing trend aggravates with the further increasing of rainfall intensity. Under the same rainfall intensity and rainfall duration, microtopographic factors of rough slope change more dramatically than those of smooth slope.There is a significant positive correlation between the variation of topographic factors and the runoff and sediment yield parameters (runoff rate, sediment rate, accumulative runoff volume, and accumulative sediment yield), but the correlation is only based on the condition of the same initial slope treatment; under different slope treatments, the variation of microtopographic factors on the slope does not correspond with the amount of soil erosion.Compared with the smooth surface, the rough surface could effectively reduce runoff yield in the early stage of rainfall, and the yield on both slopes tends to be consistent with the elongation of rainfall duration.Under four rain intensities in the experiment, the runoff rates of rough slope and smooth slope both increase at first and then tend to be stable; the sediment yield and runoff rate of rough slope display the same trend; but on smooth slope, sediment yield increases rapidly at the early stage of runoff yield, and then decreases and finally tends to be stable. The research results provide reference for studying soil erosion mechanism and establishing hillslope erosion and sediment yield model.

Key words: rainfall intensity, roughness, microtopography factors, runoff yield, sediment yield

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