裸地雨滴溅蚀对坡面微地形的影响与变化特征

    Variation characteristics and effects of splash erosion on slope micro-relief in bare fields

    • 摘要: 为了探讨溅蚀作用与坡面微地形之间的相互关系,该文通过模拟降雨试验方法,研究了黄土区坡耕地无植被条件下雨滴对坡面微地形的溅蚀作用与变化特征。微地形由不同的耕作管理措施形成,包括锄耕措施、掏挖措施和等高耕作措施,以平整坡面为对照措施。降雨强度分别为60,90和120 mm/h。试验小区大小为0.5 m2。用溅蚀板测定坡面向下和向上2个方向的溅蚀量。利用激光扫描仪测定微地形,并结合GIS技术建立大比例DEM(分辨率2 cm)。结果表明,在耕作管理条件下,坡面微地形具有降低坡面溅蚀量的作用。微地形的变化特征主要表现为微坡度的变化,而微坡向对溅蚀作用的变化不敏感。因此,微坡度可以作为研究雨滴溅蚀作用与微地形变化的一个反映指标。

       

      Abstract: In order to determine the effect of migration distance on the abrasion degree of red soil aggregate in different layer in overland flow, the relationship between aggregate stability of red soil in different layer and abrasion degree was studied based on the analysis of aggregate stability and the simulated scouring experiment in laboratory. Red soils from three areas (Xianning, Jinxian and Changsha city) were chosen for this study. The results showed that the aggregate stability of red soils from wetting sieving and LB methods (fast-wetting and stirring pre-wetted) was the greatest for iron-manganese illuvial layer, intermediate for reticulated mottling layer and least for the surface soil layer in the three areas. However, the slow-wetting treatment had no significant regularity between the different layers in this study. The main mechanisms of aggregate breakdown in different layers were slaking and mechanical breakdown. The abrasion degree of aggregate in different layers was iron-manganese illuvial layer < reticulated mottling layer < surface soil layer in five migration distances. The parameter RMI which describes mechanical breakdown showed a significant correlation with the abrasion degree and abrasion coefficient α. By introducing the parameter RMI and transport distance x, the abrasion degree prediction equation of red soil aggregate in different layer was established with a good correlation coefficient (R2= 0.88). The equation showed a good prediction performance. The results can provide a reference for research on erosion mechanisms of red soil, which is of great significance for the development of adequate soil erosion models.

       

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