四川紫色土地区鹤鸣观小流域分布式侵蚀产沙模型
收稿日期: 2006-01-18
修回日期: 2006-05-28
网络出版日期: 2006-12-15
基金资助
国家自然科学基金资助项目(40271075);长江水利委员会水土保持局支持项目
A distributed model of soil erosion and sediment yield for Hemingguan watershed in the purple soil area of Sichuan
Received date: 2006-01-18
Revised date: 2006-05-28
Online published: 2006-12-15
袁再健, 蔡强国, 褚英敏, 冯明汉, 李双喜 . 四川紫色土地区鹤鸣观小流域分布式侵蚀产沙模型[J]. 地理研究, 2006 , 25(6) : 967 -976 . DOI: 10.11821/yj2006060003
The area of the Sichuan Basin is 1.58×105km2 and purple soil is the dominant soil type in the hilly areas of the basin,but the area of soil and water loss is 7.71×104 km2,and the lost surface soils are up to 3.77×108 tons annually.Because the erosion models in China are almost empirical and the research regions mainly focused on the Loess Plateau,it is difficult to popularize such models.This paper took Hemingguan watershed of Nanbu County in Sichuan Province as a case and constructed a distributed model for soil erosion and sediment yield according to the aggravation status of soil and water loss in the purple soil region. This model takes grid as calculated unit with a resolution of 20 m×20 m.It takes 10 minutes as a time-step,simulates runoff and erosion process of rainfall in each cell,calculates the amount of runoff,erosion and sedimentation in each cell,and finally,calculates runoff and erosion of the whole watershed by recursion algorithm for single rain event.Moreover,the model can quantitatively analyze the degree of soil and water loss and evaluate the effect of variation of land use,water conservation measures and support practice on runoff.The model was finally validated in Hemingguan watershed,and the results showed that the proposed model could reasonably simulate rainfall-runoff and erosion in the watershed. This model considered the effect of soil and runoff by other cells and used stream power to simulate the modulus of erosion.By the way,the model considered slope factor and the effect of vegetation coverage on erosion and roughly calculated the gully erosion.So,the mechanism of the model is impersonal.Furthermore,the parameters of the model can be easily obtained and the computer manipulation is simple.The model can be applied to similar watersheds(i.e.,with similar climate and conditions of underlying surface) and the structure or principle of the model can be used as a reference to other regions.
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