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基于双土槽试验研究的黄土坡面侵蚀产沙过程
引用本文:肖培青,郑粉莉,贾媛媛.基于双土槽试验研究的黄土坡面侵蚀产沙过程[J].中国水土保持科学,2003,1(4):10-15.
作者姓名:肖培青  郑粉莉  贾媛媛
作者单位:1. 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,712100,陕西,杨凌;黄河水利委员会黄河水利科学研究院,450003,郑州
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,712100,陕西,杨凌
基金项目:中国科学院知识创新重要方向项目"水蚀预报模型研究"(KZCX3-SW-422);国家自然科学基金项目"黄土高原小流域分布式水蚀预报模型研究"(40335050)
摘    要: 定量分析梁峁坡面各侵蚀带之间侵蚀过程中的相互作用及其影响机理,将为坡面侵蚀预报模型的建立提供重要的理论基础。利用供沙土槽和试验土槽双土槽径流小区,研究不同上方汇流含沙量、不同降雨强度和不同地表面条件下的黏黄土陡坡面(15°)上方汇流汇沙,对坡下方侵蚀产沙过程的影响。研究结果表明:上方汇流汇沙对坡面侵蚀产沙过程有重要影响,上方来沙不但被径流全部搬运,而且上方来水在试验土槽引起了净侵蚀产沙量,坡面侵蚀现象为侵蚀-搬运过程占主导地位。对于疏松土和紧实土处理,上方汇流引起坡下方的净侵蚀产沙量,分别占试验土槽全部产沙量的31.1%-97.3%和45.1%-89.7%。上方汇流引起坡下方净侵蚀产沙量随降雨强度的增加而增加,同时受土壤容重和下垫面细沟侵蚀发展过程的综合影响。土壤容重影响坡面侵蚀的发生和发展,而坡面侵蚀产沙过程与细沟发育过程相对应。

关 键 词:双土槽径流小区  上方汇流汇沙  净侵蚀产沙量  侵蚀过程
修稿时间:2003年10月13

Loess Hill Slope Erosion and Sediment Yield Process Using A Dual Box System
Xiao Peiqing,Zheng Fenli,Jia Yuanyuan.Loess Hill Slope Erosion and Sediment Yield Process Using A Dual Box System[J].Science of Soil and Water Conservation,2003,1(4):10-15.
Authors:Xiao Peiqing  Zheng Fenli  Jia Yuanyuan
Institution:1.State Key Laboratory of Soil Erosion and Dryland Fanning on Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Scienceand Ministry of Water Resourcse, 712100 Yangling, Shaanxi;2.Scientific Institute of Hydraulic Research of Yellow River, Yellow River Conservancy Commission, 450003 Zhengzhou: China
Abstract:To quantify mutual influences and mechanisms of erosion processes about different erosion zones on loess ridge -mound-slope, which will provide important theoretic basis for constructing slope erosion prediction model. So a dual-box system of feeder box and test box with 15?gradient and clay loess was used to quantify effects of runoff and sediment from up-slope on down-slope erosion process under different sediment concentrations in up-slope runoff, rainfall intensities and soil surface conditions. The experiment results showed that runoff and sediment from up-slope have significant impacts on down-slope erosion process,sediment from up-slope was wholly transported, and runoff in up-slope caused the net sediment delivery (S) , sediment regime at down-slope is erosion-transported dominated. For the loose and compact surface treatments, the net sediment delivery (S) caused by up-slope runoff accounts for the total sediment delivery (Sft) at sown-slope 31.7% to 97.3% and 45.1% to 89.7% separately. The net sediment delivery (S) increases with an increase of rainfall intensity. In addition, soil bulk density and rill erosion development have great effects on the sediment delivery (S) . Soil bulk density affects soil erosion process and the sediment delivery (S) during the run is associated with rill head-cut advance.
Keywords:dual-box system  run-on water and sediment  net sediment delivery  erosion process
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