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上黄试验区径流泥沙观测
引用本文:赵满礼,巨仁. 上黄试验区径流泥沙观测[J]. 水土保持研究, 1990, 0(1): 99-101
作者姓名:赵满礼  巨仁
摘    要:本文系“六五”试验测定资料简结,其结果为(1)坡地水土流失量随坡度增大而增大,但至临界坡度(约30°)则出现减少趋势;(2)在大致相近的坡度下(19~22°),土壤流失量农地(2312t/km2)>退耕草地(981t/km2)>封禁荒坡(67t/km2)>坡面措施植林地(19~24t/km2);(3)降雨强度大水土流失量大,一次大强度降雨(平均雨强0.46mm/min)可使水土流失量占全年流失量的60%以上。


Observations of Silt Quantity in Runoff at Shanghuang Experimental Field
Zhao Manli,Ju Ren. Observations of Silt Quantity in Runoff at Shanghuang Experimental Field[J]. Research of Soil and Water Conservation, 1990, 0(1): 99-101
Authors:Zhao Manli  Ju Ren
Abstract:This paper is a brief summary on the observations of runoff silt at Shanghuang experimental feild during the sixth five-year-plan. Observative results are as follows: l.the quantity of soil and water loss increases along with the rising of slope until the critical angle (30°); 2. at about the same slope (19~22°), the quantity of soil loss is farming land (2 312 t/km2)>grass land removing from plough (981t/km2)>closed slope(67t/km2)>slope land with vegetation(19~24t/km2); 3.the quantity increases when fall intensity of rain is high, one strengthen rain fall (the average fall intensity is 0.46mm/min) could make the loss quantity as high as 60% of whole year’s.
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