摘要
该文应用稀土元素(REE)示踪法研究土壤侵蚀发生和发展动态过程的方法,分析了土壤侵蚀沿坡面变化的规律。采用Dy、La、Sm、Yb、Ce、Eu、Nd、Tb等8个REE进行了一系列的人工降雨模拟试验,并采用3个雨强(50,100和150mm/h)和5个坡度(8.74%,17.63%,36.4%和46.63%),分、2个降雨阶段进行,定量分析了土壤表面雨水动力特征与土壤侵蚀之间的动态平衡过程,揭示了土壤侵蚀发生和发展的过程及土壤侵蚀沿坡面分布的规律,结果表明雨强和坡度越大的条件下,侵蚀率越大的区段越靠近坡的顶端,这与细沟发生的部位完全吻合。
A new idea was advanced to identify the initiation and the development of the dynamic soil erosion pro eesses with the rare earth elements （REE） method under simulated rainfall conditions. A series of experiments were conducted with Dy, La, Sm, Yb, Ce, Eu, Nd and Tb different rainfall intensity （50, 100 and 150 mm/h） and under laboratory rainfall simulator conditions at three four slope gradients （8.74%, 17.63%, 36.4% and 46. 63%）. Two consecutive rainstorms were applied with a 24 hours interval. The initiation and development of soil erosion along slope was studied. And the dynamic equilibrium of runoff and soil erosion along slope was quantitatively analyzed. This paper revealed clearly the occurrence and development processes of soil erosion, and showed the development of the rill and soil erosion along slope. The results show that soil erosion mainly occurs the upper slope with the bigger rain intensity and slope, which is consistent with the gully erosion.
出处
《农业工程学报》
EI
CAS
CSCD
北大核心
2006年第3期32-35,共4页
Transactions of the Chinese Society of Agricultural Engineering
基金
教育部科学技术研究重大项目(ZD01-10)
中国科学院"引进国外杰出人才"项目(982602)
关键词
稀土元素
模拟降雨
土壤侵蚀
rare earth element
rainfall simulation
soil erosion
