[1]刘元保,朱显谟,周佩华,等.黄土高原坡面沟蚀的类型及其发生发展规律[J].水土保持研究,1988,(01):9-18.
Liu Yuanbao,Zhu Xianmo,Zhou Peihua,et al.The Laws of Hillslope Channel Erosion Occurrence and Development on Loess Plateau[J].Research of Soil and Water Conservation,1988,(01):9-18.
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Liu Yuanbao,Zhu Xianmo,Zhou Peihua,et al.The Laws of Hillslope Channel Erosion Occurrence and Development on Loess Plateau[J].Research of Soil and Water Conservation,1988,(01):9-18.
黄土高原坡面沟蚀的类型及其发生发展规律
《水土保持研究》[ISSN:1005-3409/CN:61-1272/P]
卷:
期数:
1988年01期
页码:
9-18
栏目:
出版日期:
1900-01-01
- Title:
- The Laws of Hillslope Channel Erosion Occurrence and Development on Loess Plateau
- 摘要:
- 沟壑纵横是黄土高原的一大特点，复杂的沟系和沟蚀在黄土高原土壤侵蚀中占有重要的地位。我们将纵横的沟槽分为三个系列。将坡面侵蚀沟系列分为细沟、浅沟、切沟三个类型进行研究，给浅沟下了新的定义，把集流槽划为一种特殊地形，切沟按发生部位和规模大小分别分为两类，讨论了它们与冲沟、干沟的区别和鉴别方法。对坡面沟蚀的发生、发展，调查方法和控制方法等做了细致的研究。
- Abstract:
- Complex channel system,and channel erosion play a very important role in soil erosion on loess plateau.We divided the channel into three series,and subdivided hillslope erosion ditch series into rill,shallow-gully and gully.In this paper,we give shallow-gully a new defination. According to the place and sizes,we divided gully into bottom-gully, slope side gully,big gully and small gully,then,discuss the different between gully and ravine and canyon and the method of how to distinguish them.On this hasps we studied the occurrence and development and the method of survey and the control of channel erosion.
参考文献/References:
[1] 朱显谟:黄土区土壤侵蚀分类, 《土壤学报》, 1956年4卷2期.
[2] Haan, C. T. and H. P. Johaton and D. L. Brakensiek, Hydrologic Modeling of Small Watershed, American Society of Agricultural Engineers, pp299, 1982.
[3] Bennett, H. H, Element of Soil Conservation, Second Edition, McGRAW-HILL Publishing Company LTD. London, 1955.
[4] 罗来兴:划分晋西、陕北、陇东黄土区域沟间地沟谷的地貌类型, 《地理学报》, 1956年22卷3期, 201-222页.
[5] 辛树帜、蒋德麟等:《中国水土保持概论》, 农业出版社, 1982年, 53页.
更新日期/Last Update:
1900-01-01