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不同植被类型下坡面径流侵蚀产沙差异性
引用本文:于国强,李占斌,裴亮,李鹏. 不同植被类型下坡面径流侵蚀产沙差异性[J]. 水土保持学报, 2012, 26(1): 1-5,11
作者姓名:于国强  李占斌  裴亮  李鹏
作者单位:1. 中国地质调查局西安地质调查中心,西安710054/西北大学地质学系,西安710069
2. 中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西杨凌712100/西安理工大学西北水资源与环境生态教育部重点实验室,西安710048
3. 中国科学院地理科学与资源研究所陆地水循环及地表过程重点实验室,北京,100101
4. 西安理工大学西北水资源与环境生态教育部重点实验室,西安,710048
基金项目:中国科学院、国家外国专家局创新团队国际合作项目“流域水土过程模拟”;国家自然科学基金项目(40872208);国家自然科学基金项目(40971161);中国博士后基金项目(2011M501445);国土资源部科研专项(201111020)
摘    要:利用野外模拟降雨试验分析不同植被类型不同雨强下坡面降雨入渗产流和侵蚀产沙过程特征及径流侵蚀产沙差异性,阐明了不同植被类型对坡面降雨侵蚀产沙过程的调控机理及其差异。结果表明:荒地、草地和坡耕地坡面产流产沙过程线均较林地强烈,呈现出多峰多谷的特点;植被类型和雨强及二者的交互效应均对产沙有显著影响,植被类型的作用大于雨强,交互效应相对较弱;植被类型和雨强对径流有显著影响,植被类型的作用大于雨强,此时交互效应的影响并不显著。各种类型的产沙量均存在显著差异,除荒地和草地两者径流量无明显差别外,其他两者之间存在显著差异。林地具有蓄水减沙的水土保持功效,草地具有直接拦沙的水土保持功效,植被对有效控制水土流失至关重要。该项研究有助于更好地理解植被、降雨和侵蚀之间的相互关系。

关 键 词:水土保持  植被类型  径流侵蚀差异  水土保持措施功效

Difference of Runoff-Erosion-Sediment Yield Under Different Vegetation Type
YU Guo-qiang,LI Zhan-bin,PEI Liang,LI Peng. Difference of Runoff-Erosion-Sediment Yield Under Different Vegetation Type[J]. Journal of Soil and Water Conservation, 2012, 26(1): 1-5,11
Authors:YU Guo-qiang  LI Zhan-bin  PEI Liang  LI Peng
Affiliation:1.Xi’an Center of Geological Survey,China Geological Survey,Xi’an 710054;2.Department of Geology, Northwest University,Xi’an 710069;3.State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Resources, Yangling,Shaanxi 712100;4.Key Laboratory of Northwest Water Resources and Environment Ecology of MOE, Xi’an University of Technology,Xi’an 710048;5.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101)
Abstract:Though the field simulated rainfall experiments,the characteristics and regulation of,as well as the difference of runoff and erosion sediment among,the slope rainfall-induced processes of infiltration,runoff generation,erosion and sedimentation under vegetation types and rainfall intensity were analyzed,the mechanism and variance of vegetation types regulating on the runoff and sediment process were clarified.The results show that slope runoff generation and sedimentation processes under wasteland,grassland and slope farmland conditions were stronger than those under forest conditions and showed multiple peaks and valleys.The vegetation types,rainfall intensity and interaction effect on sediment were significant.The sequence of influence was vegetation types,rainfall intensity and interaction effect.The vegetation types and rainfall intensity effect on runoff were important,the vegetation type’s influence was more significant than rainfall intensity,and interaction effect was little.The difference of sediment was significant under vegetation types,and it was also similar to the difference of runoff except under wasteland and grassland.Forest’s soil and water conservation function was based on water storage and sediment reduction.Grassland’s soil and water conservation function was based on direct sediment interception,and vegetation played a very important role in soil erosion control.The information of this study can be useful for better understanding the relationships between vegetation,soil erosion and precipitation.
Keywords:water and soil conversation  vegetation types  runoff erosion difference  water and soil conversation measure function
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