摘要
土壤风蚀方程自1965年由美国学者伍德拉弗(N .P .Woodruff)和西多威(F.H.Siddoway)提出来以后,已经过多次改进和不断完善。目前,该方程已在欧美许多国家的土壤风蚀预报、风蚀防治措施设计、土壤风蚀图的绘制以及大气污染的研究等方面得到了广泛的应用。
Based on the investigation carried out in 72 pieces of non - irrigated farmland in Jingbian County,Shaanxi Province,the paper calculates the annual latent amount of wind erosion from different pieces by using the Wind Erosion Equation put forward by two American scholars,N .P. Woodruff and F.H.Siddoway.Through comparison of the calculated results with the patterns of wind erosion on land surface,it is indicated that the results calculated by the Wind Erosion Equation are consistent with the tendency of variation of the patterns of wind erosion on land surface and may represent the actual intensity of wind erosion.It is also proven that the present quantity of crop stubble left in a field and distances between the shelter-forests can not meet the demand of wind erosion control.
出处
《中国水土保持》
北大核心
1991年第3期29-30,共2页
Soil and Water Conservation in China
