[1]张会茹,郑粉莉,耿晓东.地面坡度对红壤坡面土壤侵蚀过程的影响研究[J].水土保持研究,2009,16(04):52-54,59.
　ZHANG Hui-ru,ZHENG Fen-li,GENG Xiao-dong.Effect of Slope Gradients on Soil Erosion Process in Red Earth Hillslopes[J].Research of Soil and Water Conservation,2009,16(04):52-54,59.
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地面坡度对红壤坡面土壤侵蚀过程的影响研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 16 期数: 2009年04期 页码: 52-54,59 栏目: 出版日期: 2009-08-20
Title:
Effect of Slope Gradients on Soil Erosion Process in Red Earth Hillslopes
作者:
张会茹1,2, 郑粉莉1,2, 耿晓东2,3
1. 西北农林科技大学 资源环境学院, 陕西 杨陵 712100;
2. 黄土高原土壤侵蚀与旱地农业国家重点实验室, 中国科学院 水利部 水土保持研究所, 陕西 杨陵 712100;
3. 中国科学院 研究生院, 北京
Author(s):
ZHANG Hui-ru1,2, ZHENG Fen-li1,2, GENG Xiao-dong2,3
1. College of Resources and Environment, Northwest A & F University, Yangling, Shaanxi 712100, China;
2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, CAS & MWR, Yangling, Shaanxi 712100, China;
3. Graduate University of the Chinese Academy of Sciences, Beijing 100049, China
关键词:
红壤坡面; 坡度; 产流过程; 侵蚀过程; 模拟降雨
Keywords:
red earth hillslopes; slope gradient; runoff process; soil erosion process; simulated rainfall experiment
分类号:
S157.1
摘要:
通过室内模拟降雨试验，研究了地面坡度对红壤坡面产流过程和侵蚀过程的影响，结果表明：坡面总径流量随坡度的增大呈减小趋势，其中25°坡面比5°坡面的径流量减小22.3%；随坡度的增加，坡面产流达到稳定的历时减少。径流含沙量和坡面侵蚀产沙量随坡度的变化在5°~20°呈增大趋势，而当坡度由20°增加到25°时，径流含沙量和侵蚀产沙量随坡度的增加呈减少的趋势，即在红壤坡面，坡度对侵蚀产沙量影响存在着临界坡度， 其值变化于20°~25°之间。
Abstract:
The simulated rainfall experiment was used to quantify the effects of slope gradients on runoff and soil erosion processes on red earth hillslopes. The results showed that runoff rates decreased with an increase in slope gradients. Compared to 5° slope, runoff rate on 25° slope decreased by 22.3%. The timing of reaching stable runoff reduced with an increase of slope gradients. Sediment contents in runoff and soil loss increased when slope gradients increased from 5° to 25°, but when slope gradients changed from 20° to 25°, sediment contents in runoff and soil loss decreased. The critical slope degree on effects of slope gradient on soil erosion process and the value is between 20° and 25°.

参考文献/References:

[1] 赵其国.红壤物质循环及其调控[M].科学出版社,2002:1-7.
[2] 《中国农业土壤概论》编委会.中国农业土壤概论[M].北京:农业出版社,1982.
[3] 赵其国.我国红壤的退化问题[J].土壤,1995,27(6):281-286.
[4] 史德明,周伏健,徐朋.我国南方土壤侵蚀动态与水土保持发展趋势[J].福建水土保持,1993(3):9-13.
[5] 刘青泉,陈力,李家春.坡度对坡面土壤侵蚀的影响分析[J].应用数学和力学,2001,22(5):449-457.
[6] 靳长兴,坡度在坡面侵蚀中的作用J地理研究,1996,15(3):57-63.
[7] Musgrave G W.Quantitative Evaluation of Factors in Water Erosion: A First Approximation[J].Soil and Water Conser.,1947,2:133-138.
[8] Zingg A W.Degree and Length of Land Slope as It Affects Soil Loss in Runoff[J].Agri.Engi.,1940,21:59-64.
[9] 靳长兴.论坡面侵蚀的临界坡度[J].地理学报,1995,50(3):234-239.
[10] 郑粉莉.发生细沟侵蚀的临界坡长与坡度[J].中国水土保持,1989(8):23-24.

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备注/Memo

收稿日期:2008-05-15。
基金项目:国家重点基础研究发展计划项目“不同类型区土壤侵蚀过程及其机理”（2007CB407201）；西北农林科技大学创新团队计划项目“土壤侵蚀及其治理环境效应评价”（01140202）
作者简介:张会茹（1976-），女，陕西白水人，工程师，硕士研究生，主要从事土壤侵蚀过程与机理研究。E-mail：zhanghuiru2009@163.com
通讯作者:郑粉莉（1960-），女，博士，研究员，博士生导师，主要从事土壤侵蚀过程、预报模型、侵蚀环境效应评价研究。E-mail：flzh@ms.iswc.ac.cn

更新日期/Last Update: 1900-01-01