摘要
以土石山区径流小区所产生的径流量和侵蚀量为研究对象,对在山东省临朐县辛庄试验站径流小区坡长为10 m,20 m和40 m多年的观测资料,分析了坡长与径流和侵蚀的关系。研究表明:不同坡长条件下降雨量与径流量和侵蚀量呈线性关系,同一坡长条件下,径流量和侵蚀量随降雨量的增加而增加,不同坡长条件下,随坡长的增加,径流量逐渐增加,在P【10 mm时20 m坡长的侵蚀量大于40 m坡长的侵蚀量,在P】10 mm时呈相反变化。不同坡长条件下I30与径流量和侵蚀量呈幂函数关系,同一坡长条件下,径流量和侵蚀量随I30的增加而增加,不同坡长条件下,随坡长的增加,侵蚀量逐渐增加,在I30【20 mm时20 m坡长的径流量大于40 m坡长的径流量,在I30】20 mm时呈相反变化。
The relationship between slope length and runoff with soil erosion is analyzed using years of observation data in Linqu county,Shandong province Daxinzhuang station runoff plots.The results show that rainfall and runoff with erosion is linear under different slope length,however,the runoff and soil erosion increase with the rainfall increasing on the same slope length,the runoff increases with the slope length increasing.Soil erosion of 20 m-long plot is less than 40 m-long plot's as P<10 mm,but on the contrary as P>10 mm.There is significant linear relationship between every rainfall and runoff or soil erosion.There is significant power function between the biggest of I30 rainfall intensity and runoff or soil erosion.the runoff and soil erosion increase with I30 increasing on the same slope length,soil erosion increases with the slope length increasing,and 20 m-long plot of runoff is more than 40 m-long plot's as I30<20 mm,it has contray chang as I30>20 mm.
出处
《水土保持研究》
CSCD
北大核心
2007年第A04期190-193,196,共5页
Research of Soil and Water Conservation
基金
山东省水利厅资助项目“山东典型侵蚀区水土流失机理与综合治理效益研究”
关键词
坡长
径流
侵蚀
降雨量
降雨强度
slope length
runoff
soil erosion
rainfall
rainfall intensity
