中文摘要：

研究细沟形态发育过程对认识细沟侵蚀具有重要作用,该文采用6种坡度（2°、4°、6°、8°、10°、12°）,5种流量（8、16、24、32、40 L/min）下的组合冲刷试验,系统研究了坡面细沟横纵断面形态发育影响机制及动力特性。结果表明：细沟宽深比变化范围为3.006-4.884,根据水力最佳断面,细沟水流远未达到稳定。横断面形态系数随坡度的变化范围为0.36-0.522,细沟横断面形态随流量、坡度以及冲刷历时均趋近于梯形水力最佳断面,即阻力最小的断面。随着流程长度的增加,横断面形态由宽深逐渐变窄,横断面形态系数也随之减小。细沟纵断面形态范围为0.60-11.26,且随坡度的增大而增大,与流量相关性不大。综合阻力系数及消能率均与细沟纵断面形态系数呈良好的幂函数关系。

英文摘要：

Rill erosion is the process of soil particles separating in the groove and handling by rill flow, and it is one type of surface corrosion, and the rill formed can be completely filled by normal farming activities. In the loess plateau region, rill erosion of slope accounts for more than 70% of the total erosion, and rill erosion is a major erosion in the loess plateau hilly land, and is also an important part of mechanism of slope erosion prediction. Rills are small channels which function as both sediment sources and sediment transport vehicles on hill slopes. It is a quantum leap during the process of soil erosion on slopes, and is also the beginning of qualitative changes in the process of soil erosion. The rill morphology development plays an important role in the understanding of rill erosion. Rill morphology changes have many influence factors in the process of rill erosion, so systematically studying the relationship between rill shape coefficient and influencing factors can make us better understand the process of rill erosion and erosion mechanism. For the study of rill morphological development process, the combination scouring tests of 6 slopes （2~, 4~, 6~, 8~, 10~, and 12~） and 5 discharges （8, 16, 24, 32, and 40 L/min） were carried out, and the effect mechanism of rill transverse profile morphological development on the loess slope surface was investigated, as well as the dynamic characteristics of the impact. The results showed that rill width-depth ratio ranged from 3.006 to 4.841, and according to the hydraulic optimum section, the rill flow was far from steady state. In rill erosion, downward erosion and lateral erosion gradually transited to downward erosion. Because of incised and lateral erosion, rill cross-sectional shape was gradually widened and deepened with the increase of slope and time. Along with the change of slope, cross-sectional shape coefficient varied within the range of 0.36-0.522. Research showed that： The rill cross-sectional shape was approximating to the trapezoida