[1]江忠善,李秀英.黄土高原土壤流失预报方程中降雨侵蚀力和地形因子的研究[J].水土保持研究,1988,(01):40-45.
　Jiang Zhongshan,Li Xiuying.Study on the Rainfall Erosivity and the Topographic Factor of Predicting Soil Loss Equation in the Loess Plateau[J].Research of Soil and Water Conservation,1988,(01):40-45.
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黄土高原土壤流失预报方程中降雨侵蚀力和地形因子的研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 期数: 1988年01期 页码: 40-45 栏目: 出版日期: 1900-01-01
Title:
Study on the Rainfall Erosivity and the Topographic Factor of Predicting Soil Loss Equation in the Loess Plateau
作者:
江忠善, 李秀英
Author(s):
Jiang Zhongshan, Li Xiuying
摘要:
通用土壤流失方程已在许多国家研究推广应用。本文根据黄土高原的以往径流小区实测资料，分析提出了适合于这一地区的土壤流失方程的降雨侵蚀力指标和地形因子的关系式，文中还就我国设立标准小区的选用规格提出了看法。
Abstract:
In this paper,the rainfall erosivity factor R and the relations of topographical factor LS in the loess region have been studied.This analytical results showed that the product EI30 of rainfall kinetic energy E and maximum 30-rain rainfall intensity I30 is a good-rainfall erosivity index which closely related with the soil loss on bare fallow land, hut it is better to select all individual rainfalls that greater than or equal to ten millimetres as the estimates of rainfall erosivity factors for a year or average annual.The relation of topographical factor LS can be used to estimate the effects of topographical factors in the loess region.

参考文献/References:

[1] Wischmeier, W. H. and D. D. Smith:Rainfall energy and its relationship to soil loss, Trans. of the Amer, Geophysical Union, Vol, 39, pp 285-291, 1958
[2] 江忠善等:黄土地区天然降雨雨滴特性研究, 《中国水土保持》, 1983年第3期, 第32-36页.
[3] Foster, G. R, F, Lombardi and W. G, Moldenhauer, Evaluation of rainfall-runoff erosivity factors for individual storms, Trans, of the ASAE, Vol, 25, pp124-129, 1982.
[4] Wischmeier, W. H, and D. D. Smith, Predicting rainfall erosion losses from cropland east of the Rocky Mountains, USDA, Agr. Handbook No. 282, 1965.

更新日期/Last Update: 1900-01-01