摘要
黄土丘陵区的沟间地面积一般占50%左右,通过比较分析,提出用系统分析法来计算小流域沟间、沟谷地的产流产沙量。结果发现沟间地侵蚀量占40%左右,沟谷地占60%左右,沟间沟谷地产流量接近,但沟间地径流下沟最少能使沟谷地侵蚀量增加1倍,因而,沟间地径流造成的侵蚀量占全流域的70%左右。
In loessal hill region, the intergully land is about 50% of the total area. Through the comparison and analysis, a method of system analysis is put forward to calculate the runoff and sediment quantity of gully and inter-gully land in small watershed. It is found that the erosion of gully and intergully land is respectively about 60% and 40% of the total. The runoff yields between this two land types are nearly equal, but a half of the gully erosion, at least, is caused by intergully runoff flowing down the gully, so there is 70% of the total erosion which is caused by intergully runoff.
出处
《水土保持学报》
CSCD
北大核心
1992年第2期24-28,共5页
Journal of Soil and Water Conservation
关键词
黄土丘陵区
泥沙来源
小流域
loessal hill region gully and intergully land runoff and sedinent source