Types of Bank Slope and Its Stability form Yibin to Baihetan on Jinsha Rive

By researching the locale and studying geologic background and rock-mechanics surroundings on hyroeijectric zone of Jinsha river(Yibing-Baihetan),the authors divide bank slopes into 9 types according to structure of rock and soil and terrain,and expatiate the distributing character and stability of each bank slope types,which serves as scientific geo-accordings in forecasting and controlling of bank slope's unsteady on hyroeijectric zone of Jinsha river.     

Experimental Analysis of Deformation Characteristic for Soil Bank Slope Under Reservoir Water Level Fluctuation

Under reservoir water level fluctuation, soil bank slope water sucking, stress concentration and slip deformation in Three Gorges Reservoir area form slope cracks system at different periods and different spatial parts. In this study, laws of cracks spatial evolution in different deformation periods for soil bank slope were analyzed during a water cycle of impoundment and decline by model test. The test results indicated that, in the initial impoundment period, cracks appeared near the water line at the bank slope leading edge with high appearance frequency, and scale increased gradually and partial bank slope collapsed and damaged. In the middle impoundment period, cracks appeared in the front and trailing edges of bank slope, the frequency of occurrence and the scale of which decreased. And in the late impoundment period, the leading edge of the cracks development disappeared, the trailing edge of the cracks continued to develop and the bank slope crept along the sliding surface as a whole. Cracks expanded slowly in the pause impoundment as the water level raised. In the water level decline stage, tensile cracks mainly occurred in the back edges of bank slope. In the early water level decline, cracks appeared in low frequency and it grew slowly. In the late water level decline, cracks appeared in high frequency and large scale, and where the bank slope produced lower seat deformation and dislocated berm. Moreover, in water level decline stage, bank slope crept along the sliding surface as a whole.     

Stability Analysis on Excavated High Slope of Mozong River Power Station in Wulong

The subject matter of this paper is to analyze the stability of excavated high slope. On the base of typical engineering case in Wulong, Chongqing, the geological conditions and potential failure pattern of the high slope are discussed. Then, the limit equilibrium method and the stereographic projection method are used to synthetically analyze the stability of excavated high slope. As a result, it indicates that the stability of the high slope in insufficient and some retaining structures ought to be adopted for the high slope as soon as possible.     

Effect of Concentrated Leachate Recirculation on Leachate Level and Slope Stability of Municipal Solid Waste Landfill

260 tons concentrated leachate per day is produced at the leachate treatment plant at Changan landfill, which is considered to be recirculated into the landfill of municipal solid wastes. The effect of leachate recirculation on the slope stability of the landfill should be evaluated. The results from engineering geology and hydrogeology survey were firstly presented. Three-dimensional unsaturated-saturated seepage analyses were carried out by using GMS software to predict the change of leachate level as a result of the leachate recirculation. Based on the leachate levels and pore-water pressures obtained from the seepage analyses, slope stability analyses were carried out to evaluate the safety of the landfill. Some control measures were proposed to eliminate the adverse effect of leachate recirculation on the landfill safety. The analyses indicate that the factor of safety (FS) for the landfill with the current leachate level is slightly greater than the safety requirement (FS=13), and the current leachate level happens to be the critical level. Direct leachate recirculation will result in a significant rise in leachate level, which will cause a significant decrease in the landfill safety. The landfill is likely to fail after a direct leachate recirculation. If the leachate recirculation is executed after the current leachate level is lowered down by 3 m and the resultant leachate level will be lower than the current leachate level, the landfill can remain safe. Vertical pumping wells are proposed to implement the drawdown work, and if 45 wells are used and pumping is conducfed for 3 mouths, the leachate level will decrease by 3 m, which meets the safety requirement.     

降雨入渗对宁南山区黄土梯田边坡稳定性的影响

为了研究降雨入渗对宁南山区黄土梯田边坡稳定性的影响。采用ABAQUS软件建立降雨入渗下的宁南山区黄土梯田边坡稳定性有限元模型,研究了水平梯田、隔坡梯田、原始边坡（对照）3种边坡类型,在降雨入渗强度(28~38 mm/h)和边坡坡度(15°—30°)下的破坏时间和安全系数的变化规律。结果表明:降雨入渗下,黄土梯田边坡的破坏时间随降雨入渗强度的增大而减小,且呈幂函数关系,水平梯田的破坏时间显著高于隔坡梯田和原始边坡;安全系数也随降雨入渗强度的增大而减小,但呈线性关系,水平梯田的安全系数与隔坡梯田和原始边坡并无显著差异。降雨条件下,修筑梯田能增加浅层梯田边坡的稳定性,而对于深层梯田边坡的稳定性影响不大。     

Stability Analysis for the Excavation Engineering Under Coupling Effect of Seepage from Heavy Rain and River Fluctuation

The seepage accident is very easily occurred, when the excavation engineering has been constructed in rainy season and it is very easily influenced by the coupling effect of seepage duo to heavy rain and water level fluctuation of neighboring river. So a coupling seepage equation that based on the theory of Dupuit has been established for the ground water in the layered foundation. And then, the water table surrounding the excavation engineering has been determined on the consideration of the coupling effect of seepage duo to heavy rain and water level fluctuation of river. In the meantime, by means of the theory of coupling analysis of stress and seepage and the software of Midas, a model of coupling analysis of stress and seepage has been built for the specific excavation engineering and the seepage destroy characteristics of this project has been researched.     

台风“凤凰”路径强度变化对太湖北岸风雨影响的诊断

为探讨2014年第16号台风“凤凰”运动路径怪异和数次登陆强度不变的特点,了解其给太湖北岸地区带来的风雨影响,通过对台风环境背景场的天气学分析和物理量诊断,对16号台风“凤凰”的路径动态、强度变化、结构特征进行分析。结果表明：受副高进退和引导气流作用,台风“凤凰”沿着副高外围,先后经历西进、北上,东出的运动,深层引导气流能较好的指示台风的运动。台风“凤凰”自身体积较小,发生发展前期海温偏低,海洋热容量低,温度条件不利于台风的增强。同时,台风流场结构极为不对称,随着垂直风切的增强,台风强度减弱,并经过数次登陆,破坏了环流结构,总体强度难以增强。由于台风路径偏东,强度偏弱,影响范围较小,水汽输送条件不利,且无冷空气配合,太湖北岸地区在此次台风过程中以中雨为主,风力影响集中在台风环流中心附近,影响总体较小。