[1]郑世清,周佩华.土壤容重和降雨强度与土壤侵蚀和入渗关系的定量分析[J].水土保持研究,1988,(01):53-56.
Zheng Shiqing,Zhou Peihua.A Quantitative Study of Relationship Between Soil Density and Soil Erosion[J].Research of Soil and Water Conservation,1988,(01):53-56.
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Zheng Shiqing,Zhou Peihua.A Quantitative Study of Relationship Between Soil Density and Soil Erosion[J].Research of Soil and Water Conservation,1988,(01):53-56.
土壤容重和降雨强度与土壤侵蚀和入渗关系的定量分析
《水土保持研究》[ISSN:1005-3409/CN:61-1272/P]
卷:
期数:
1988年01期
页码:
53-56
栏目:
出版日期:
1900-01-01
- Title:
- A Quantitative Study of Relationship Between Soil Density and Soil Erosion
- 摘要:
- 本文根据人工模拟降雨试验方法，在不同土壤容重，同等坡度和同级降雨强度条件下，以及同种土壤容重，不同降雨强度条件下，对土壤侵蚀和土壤入渗关系进行了定量分析。
- Abstract:
- In this paper,soil erosion and soil infiltration were quantitatively studied under artificial rainfall simulator with the different treatments, such as combination of different soil bulk densities with the unvaried steepness and the unvaried rainfall intensity,and the combination of the unvaried soil bulk density with different rainfall intensities. The experimental results indicated that soil loss and the capacity of soil infiltration decreased with increase in soil bulk density.Soil bulk density was highly relative to soil erodibility.Although the different rainfall intensities had some effects on the capacity of soil infiltratiori, their relativity was not significant.
参考文献/References:
[1] 蒋定生等:地面坡度对降水入渗影响的模拟试验, 《水土保持通报》, 1984年4期, 10-13页.
[2] 田积莹等:黄土地区土集物理性质及黄土成因的关系, 《中国科学院西北水上保持研究所集刊》, 1987年, 第6集, 1-12页.
[3] 李玉山等:黄土高原土城水分性质及其分区, 《中国科学院西北水土保持研究所集刊》, 1985年第2集, 1-17页.
[4] 郑世清等:坡地开垦对水土流失的影响, 《水土保持通报》, 1986年8期, 55-56页.
更新日期/Last Update:
1900-01-01