不同降雨条件下垄作坡面地表微地形及土壤侵蚀变化特征  

Characteristics of variations in soil surface micro-topography and soil erosion on the cross ridge slope under different rainfall conditions

作　　者：林艺[1] 秦凤[1] 郑子成[1] 张林[1] 刘麟翔 徐巍[1] 吴春柳[1] 李廷轩[1] 

机构地区：[1]四川农业大学资源学院,成都611130

出　　处：《中国水土保持科学》2015年第3期32-38,共7页Science of Soil and Water Conservation

基　　金：国家自然科学基金"紫色土坡耕地侵蚀演化特征及其对作物防蚀的响应机制"(41271307);"川中丘陵区坡耕地防蚀机理研究"(40901138);四川省教育厅项目"紫色土区玉米季横垄坡面片蚀过程研究"(15ZB0009);四川农业大学大学生创新性实验计划项目"紫色土垄作条件下地表糙度的侵蚀效应"(1310626087)

摘　　要：为了弄清垄作坡面地表微地形的变化及土壤侵蚀特征,以期有效防控紫色土区坡耕地水土流失,通过室内人工模拟降雨试验,分析递增和递减降雨系列下,紫色土区横坡垄作坡面地表微地形的空间变化特征,探讨其对地表产流和侵蚀产沙的影响。结果表明：1）在不同降雨条件下,地表高程变化均以减小为主,变化量主要集中在-2~0cm之间。2）递增降雨条件下,地表糙度在前2场降雨中无明显变化,到第3场降雨后明显增大;递减降雨条件下则先增大后减小。3）不同降雨条件侵蚀产沙量差异不大,递增降雨条件下产沙量比递减条件下大3.9%;但产流量比递减条件下小14.8%。4）递增降雨较递减降雨产流、产沙时间更晚。5）横坡垄作在小降雨强度时可有效地减少土壤侵蚀,但当降雨强度增大到1.5 mm/min时,则易发生断垄现象,反而会增大土壤侵蚀。The purpose of this study was to understand the characteristics of variations in soil surface micro-topography and soil erosion,providing evidence for the effective prevention and control of soil erosion in sloping farmland of purple soil region. Based on the indoor simulated rainfall experiments,the spatial variation of soil surface micro-topography was studied in sloping farmland with cross ridge in purple soil region under the conditions of increasing and decreasing rainfall series. Soil surface roughness was used to indicate the dynamic changes in the soil surface micro-topography. On this basis,soil surface roughness was calculated and DEM was established,and the effect of soil surface micro-topography on runoff and sediment yield was explored. The results showed that the change of soil surface elevation was characterized primarily by the reduction in increasing and decreasing rainfall series,concentrated mainly in the range of- 2 to 0 cm. Under the increasing rainfall series,soil surface micro-topography changed obviously in the middle course of rainfall and the rill erosion kept intensifying. However, in the decreasing rainfall series,soil surface micro-topography began to collapse in earlier rainfall course. In the late rainfall course,rills tended to broaden and deepen,but the starting point of rill formation wasrelatively stable,which did not extend and develop along the ridge direction. In the increasing rainfall series,the variation of soil surface roughness was not obvious in the first two rainfalls,whereas the soil surface roughness showed a significant increase in the third rainfall. The soil surface roughness increased first and then decreased under the decreasing rainfall series. The difference of sediment yield was not significant between the increasing and decreasing rainfall series. The sediment yield in the increasing rainfall series was 3. 9% higher than that in the decreasing rainfall series,while the volume of runoff under the condition of the increasing rainfall series was 14. 8% lower th

关 键 词：降雨条件 横坡垄作 地表微地形 土壤侵蚀 

分 类 号：S157.1[农业科学—土壤学]