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坡度对侵蚀产沙及其粒径分布的影响 被引量:19

Effects of Slope Gradient on Yield and Particle Size Distribution of Sediment
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摘要 利用人工模拟降雨试验,分析北京山区普通褐土在不同坡度条件下的产流产沙状况和侵蚀泥沙的粒径分布规律。结果表明,随着坡度的增大,侵蚀模数呈现先增加后减少的趋势,临界坡度为25°,对应的侵蚀模数为19.7t/hm^2。在研究的5个坡度条件下,侵蚀泥沙都以粉粒为主。当坡度从0增大至30°,<0.002mm的粘粒含量无明显变化;0.002~0.02mm的细粉粒含量先减少后增加;0.02~0.25mm粗粉粒、极细砂粒和细砂粒含量则呈现先增加后减少的趋势。临界坡度为20°,此时细粉粒含量最少,极细砂粒和细砂粒含量最多。与原土相比,侵蚀泥沙在不同粒级存在富集。主要富集粒径随坡度增加先增大后减小。20°坡度时富集粒径最大,为细砂粒(0.1~0.25mm)。 Slope gradient is one of the important factors that affect soil erosion,which not only influences runoff and sediment yield,but also affects the size distribution of sediment particles.Quantitatively evaluating the effects of slope gradient on yield and particle size distribution of sediment is essential for studying water erosion mechanism,calculating nutrient loss,and establishing water erosion model and non-point source pollution model.In the current study,the sediment yield and particle size distribution were analyzed for a typical soil(cinnamon soil)in the mountain area of Beijing at 5different slope gradients,based on rainfall simulation experiments.The results showed that with the increasing slope gradient,sediment yield increased at first and then decreased.The critical slope gradient was 25°,with a sediment yield 19.7t/hm2.For all the 5slope gradient treatments,the eroded sediment was dominated by silt particles.When the slope gradient increased from 0to 30°,no obvious change was observed in the proportion of clay particles(〈0.002mm),while the percentage of fine silt(0.002—0.02mm)decreased at first and then increased,and the percentages of coarse silt(0.02—0.05mm),very fine sand(0.05—0.1mm)and fine sand(0.1—0.25mm)increased at first and then decreased.The lowest percentage of fine silt and the highest percentages of very fine sand and fine sand particles were observed at the slope gradient of 20°.Particle enrichment was observed in different particle size classes for different slope gradients,and the size of the most significantly enriched sediment particles increased at first and then decreased with the increasing slope gradient.The largest size was observed at the slope gradient of 20°,which was among 0.1—0.25mm(fine sand).
出处 《水土保持学报》 CSCD 北大核心 2015年第6期25-29,共5页 Journal of Soil and Water Conservation
基金 地表过程模型与模拟创新研究群体科学基金项目(41321001) 北京师范大学青年教师基金项目(2014NT04) 中央高校基本科研业务费专项(2013NT36)
关键词 坡度 侵蚀泥沙 粒径分布 人工模拟降雨 slope gradient runoff sediment particle size distribution rainfall simulation
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参考文献16

  • 1Meyer L D,Line D E,Harmon W C.Size characteristics of sediment from agricultural soils[J].Journal of Soil and Water Conservation,1992,47(1):107-111.
  • 2Walling D E,Owens P N,Waterfall B D,et al.The particle size characteristics of fluvial suspended sediment in the Humber and Tweed catchments,UK[J].The Science of the Total Environment,2000,251/252(1):205-222.
  • 3Schiettecatte W,Gabriels D,Cornelis W M,et al.Enrichment of organic carbon in sediment transport by interrill and rill erosion processes[J].Soil Science Society of America Journal,2008,72(1),50-55.
  • 4Yang Y,Ye Z H,Liu B Y,et al.Nitrogen enrichment in runoff sediments as affected by soil texture in Beijing mountain area[J].Environmental Monitoring and Assessment,2014,186(2):971-978.
  • 5Pieri L,Bittelli M,Hanuskova M.Characteristics of eroded sediments from soil under wheat and maize in the North Italian Apennines[J].Geoderma,2009,154(1/2):20-29.
  • 6吴凤至,史志华,方怒放,岳本江.不同降雨条件下侵蚀泥沙黏粒含量的变化规律[J].环境科学,2012,33(7):2497-2502. 被引量:22
  • 7张兴昌,邵明安.侵蚀泥沙、有机质和全氮富集规律研究[J].应用生态学报,2001,12(4):541-544. 被引量:53
  • 8彭怡,王玉宽,傅斌,徐佩,王道杰.紫色土流失土壤的颗粒特征及影响因素[J].水土保持通报,2010,30(2):142-144. 被引量:22
  • 9黄丽,张光远,丁树文,蔡崇法,蔡强国.侵蚀紫色土土壤颗粒流失的研究[J].土壤侵蚀与水土保持学报,1999,5(1):35-39. 被引量:68
  • 10刘和平,符素华,王秀颖,徐丽,方岚,刘宝元,路炳军.坡度对降雨溅蚀影响的研究[J].土壤学报,2011,48(3):479-486. 被引量:27

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