坡度对坡面细沟侵蚀的影响———基于三维激光扫描技术
Effects of slope gradients on rill erosion:Study based on three-dimensional laser technology
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摘要: 采用室内人工模拟降雨试验,降雨用水为纯净水,试验坡度为10°、15°、20°、25°,降雨强度为1.5 和2.0 mm/min,试验土槽分别为5 和10 m,同时采用三维激光扫描仪对降雨前后坡面进行监测,分析不同坡度对细沟侵蚀的影响。结果表明:1)坡度对坡面产沙量影响显著,二者的关系可以采用二次项式拟合,坡面产沙量随着坡度的变陡先增加后减少;2)三维激光扫描技术能够准确地计算坡面细沟发育形态数据和细沟侵蚀量,不同坡度条件下细沟发育不同,细沟宽深比随着坡度的变陡而逐渐变小;3)细沟密度、细沟侵蚀量与坡度呈正相关关系,细沟发育程度随坡度的变陡而加剧。Abstract: Indoor rain simulation experiments were conducted in this study under different slope degrees (10°, 15°, 20°, 25°), rainfall intensities using deionized water (1.5, 2.0 mm/ min) and slope lengths (5,10 m). The 3D laser scanner was employed to make real-time monitor after each rainfall event, and the effects of different slope degrees on rill erosion were analyzed. The results showed that the slope sediment yield significantly correlated with slope and could be expressed by binomial fomular. As the increased slope degree, the slope sediment yield increased firstly and then declined. The 3D laser scanner could calculate the data of rill development form and erosion amounts accurately. The development of the rill differed in slopes. The ratio of rill breadth to depth became smaller with steeper slope. There was significant positive correlation between rill density, rill erosion and the slope. The development degree of rill aggravated with steeper slope.