[1]王飞,杨勤科,李锐,等.黄土高原沟槽侵蚀与泥沙输移监测方法初探[J].水土保持研究,2004,11(02):87-89.
　WANG Fei,YANG Qin-ke,LI Rui,et al.Groove Erosion in Loess Plateau and the Monitoring Methods of Groove Erosion and Sediment Delivery Ratio[J].Research of Soil and Water Conservation,2004,11(02):87-89.
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黄土高原沟槽侵蚀与泥沙输移监测方法初探

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 11 期数: 2004年02期 页码: 87-89 栏目: 出版日期: 1900-01-01
Title:
Groove Erosion in Loess Plateau and the Monitoring Methods of Groove Erosion and Sediment Delivery Ratio
作者:
王飞, 杨勤科, 李锐, 张晓萍
中国科学院水利部水土保持研究所, 陕西, 杨陵, 712100
Author(s):
WANG Fei, YANG Qin-ke, LI Rui, ZHANG Xiao-ping
Institute of Soil And Water Conservation, Chinese Academy of Sciences, Yangling 712100, Shaanxi China
关键词:
沟槽侵蚀; 泥沙输移比; 监测方法; 水土保持
Keywords:
groove erosion; sediment delivery ratio; monitoring method; soil and water conservation
分类号:
S157
摘要:
沟槽是径流与输沙通道和侵蚀主体，沟槽侵蚀监测对揭示水土流失规律和进行流域产沙模拟有重要意义。在对黄土高原相关研究结果分析的基础上，对沟槽侵蚀进行了初步确定。同时对与沟槽侵蚀关系密切的泥沙输移比进行了分析，并总结出沟槽侵蚀与泥沙输移比监测和估算的沟道特征监测法、坡面产沙—出口站泥沙比较法、稀土元素示踪法、坝库泥沙还原法和经验公式拟合法等方法。
Abstract:
Groove is the channel of sediment delivery and the main body of soil erosion. Monitoring of groove erosion could not only help to know the soil erosion rules, but be very useful for the production of sediment at small watershed and regional scales. Based on some researches in the Loess Plateau, the groove erosion is described, and the meaning and usage of sediment delivery ratio are discussed. Several general monitoring and estimation methods of groove erosion and sediment delivery ratio are put forward.

参考文献/References:

[1] 陈永宗. 黄土高原地区的土壤侵蚀[A].见:孟庆枚.黄土高原水土保持[C].郑州:黄河水利出版社, 1996.148-177.
[2] 唐克丽, 熊贵枢, 梁季阳, 等.黄河流域的侵蚀与径流泥沙变化[M].北京:中国科学技术出版社, 1993.79-88.
[3] 牟金泽, 姚文艺.水土流失与泥沙输移[A].见:孟庆枚.黄土高原水土保持[C].郑州:黄河水利出版社, 1996.178-212.
[4] 陈国祥, 谢树楠, 汤立群.黄土高原地区流域侵蚀产沙模型研究[A].见:孟庆枚.黄土高原水土保持[C].郑州:黄河水利出版社, 1996.213-229.
[5] 牟金泽, 孟庆枚.论流域产沙量计算中的泥沙输移[J].泥沙研究, 1982, 1(2):60-65.
[6] 陈永宗.黄土高原沟道流域产沙过程的初步分析[J].地理研究, 1983, 2(3):35-46.
[7] 王飞, 李锐, 杨勤科.土壤侵蚀研究的尺度转换[J].水土保持研究, 2003, 10(2):9-12.
[8] Ferro, V, Minacapilli, M.Sediment delivery processes at basin scale[J].Hydrological Sciences Journal, 1995, 40(6):703-718.
[9] 蔡强国, 陆兆熊, 王贵平.黄土丘陵沟壑区典型小流域侵蚀产沙过程模型[J].地理学报, 1996, 51(2):108-117.
[10] 唐小明, 李长安.土壤侵蚀速率研究方法综述[J].地球科学进展, 1999, 14(3):274-278.
[11] 卜兆宏, 刘绍清.土壤流失量及其参数实测的新方法[J].土壤学报, 1995, 32(2):210-220.

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备注/Memo

收稿日期:2004-2-25。
作者简介:王飞（1971- ），男，陕西户县人，助理研究员，博士研究生，从事区域水土保持与环境研究，已经发表论文10多篇.

更新日期/Last Update: 1900-01-01