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| 1 | 地震作用下含倾斜软弱夹层斜坡场地的动力响应特性研究显示文摘以四川北部龙门山断裂带附近山区内某核废料处置场为参考原型,概化出含软弱夹层的斜坡场地模型,设计完成该特殊场地在50倍重力加速度条件下的离心振动台模型试验,监测场地在不同输入地震工况下的加速度响应,重点通过加速度放大效应和地震波波动机制探讨软弱夹层和斜坡效应对斜坡场地动力响应的影响,此外,结合传统傅里叶谱和Hilbert边际谱方法,从频域角度展示场地的频谱变化特性。试验结果表明:软弱夹层的加速度放大效应与输入地震动峰值有关,当输入地震动峰值较小时,夹层内响应加速度峰值被削弱,当输入峰值较大时,则被增强;斜坡效应对该场地中软弱夹层内的动力响应存在影响,导致斜坡下的软弱夹层内加速度放大效应增强;随着输入地震动峰值增大,软弱夹层中响应加速度的频率成分发生了变化,高频成分减少而低频成分增加。 | 闫孔明 刘飞成 朱崇浩 王志佳 张建经 | 2017 | 岩石力学与工程学报2017，36，11： | 18 |
| 2 | 悬臂式抗滑桩加固黏土边坡地震永久位移算法显示文摘为了有效地确定悬臂式抗滑桩加固的黏土边坡地震永久位移,基于极限分析上限定理,针对圆弧滑动式土坡破坏模式,通过对设置抗滑桩条件下土坡进行外力功率和内能耗散率的计算,按严格力学定义推导出坡体在地震作用下的安全系数,进而导出与安全系数相对应的边坡地震屈服加速度计算公式,并结合Newmark滑块位移法对边坡产生的转动加速度进行二次积分,推导出与边坡设计安全系数密切相关的坡体地震永久位移的详细计算公式。以5.12汶川地震卧龙测站东向地震波为例,通过对一算例边坡进行分析,给出了边坡永久位移时程曲线以及不同设计安全系数与永久位移的关系,分析了算法与Ambraseys算法的结果,验证了所提计算方法的有效性,并得到不同设计安全系数时边坡土体黏聚力和内摩擦角对坡体永久位移的影响规律。研究结果表明,坡体永久位移随着设计安全系数的增加逐渐呈指数函数式减小变化,在较低设计安全系数下,坡体永久位移受土体抗剪强度参数影响较为敏感,随着设计安全系数的提高,这种敏感性则逐渐降低。 | 肖世国 祝光岑 | 2013 | 岩土力学2013，34，5： | 11 |
| 3 | Analysis on the Dynamical Process of Donghekou Rockslide-Debris Flow Triggered by 5.12 Wenchuan Earthquake显示文摘Among the geo-hazards caused by the great Wenchuan Earthquake, the rapid and long runout rockslide-debris flow is of primary concern due to the large volume of displaced material and the resultant catastrophic impacts to the landscape and socioeconomic structure. In order to analyze the dynamical process of this kind of geo-hazard, the Donghekou rockslide-debris flow is given as an example in this paper. This event, which killed 780 people, initiated at an elevation of 1300 m with a total long run-out distance of more than 2400 m. The slide mass is mainly composed of dolomite limestone and siliceous limestone of Sinian system, together with carbon slate and phyllite of Cambrian. During the processes from slide initiation to the final cessation of slide movement, five dynamic stages took place, here identified as the initiation stage, the acceleration of movement stage, the air-blast effect stage, the impact and redirection stage and the long runout slidematerial accumulation stage. Field investigations indicate that due to the effects of the earthquake, the dynamics of the Donghekou rockslide-debris flow are apparently controlled by geologic and tectonic conditions, the local geomorphological aspects of the terrain, and the microstructural and macroscopic mechanical properties of rocks which compose the slide mass. These three main factors which dictate the Donghekou rockslide-debris flow dynamics are discussed in detail in this paper, and significant results of field investigations and tests of materials are presented. The above dynamical processes are analyzed in this paper, and some useful conclusions have been gained. | SUN Ping ZHANG Yongshuang SHI Jusong CHEN Liwei | 2011 | Journal of Mountain Science2011，8，2： | 8 |
| 4 | 汶川地震中国道G213左侧某典型高山河谷场地地震滑坡响应分析显示文摘以国道G213左侧一处包含河谷地形的高陡边坡为原型,采用新型离散元计算方法——基于连续模型的离散元方法(CDEM),对高烈度地震作用下高陡边坡上的堆积体滑坡由变形累计到破坏滑动的全过程进行模拟,并结合振动台试验结果,对该高陡边坡上堆积体的地震滑坡响应进行研究。研究结果表明,在地震力和重力作用下,堆积体顶部先出现应力集中,造成堆积体沿基岩–堆积体结构面后缘产生变形,进而造成该处出现拉伸、剪切破坏点,之后随着地震动的持续,基岩–堆积体结构面上的剪切破坏点逐渐向堆积体中前部的锁固段扩展,同时伴随着堆积体表面拉伸破坏点的增加,最终造成锁固段发生渐进性破坏,堆积体从剪出口滑出形成滑坡。滑塌发生的时间与地震动峰值加速度到达的时间同步或稍微有所滞后。在高陡边坡地形中,以输入地震波为基准,不论是坡面还是坡体内,不同位置的峰值加速度沿坡高均有所放大,表现为竖向峰值加速度的放大效应>水平峰值加速度的放大效应,坡面峰值加速度的放大效应>坡体内峰值加速度的放大效应。在河谷地形中,以输入波为基准,不论是河床还是河岸两侧的斜坡,不同位置的峰值加速度沿高程均具有不同程度的放大;河谷对加速度放大效应的影响具有一定范围,且在该范围内水平加速度的放大效应>竖向加速度的放大效应,与坡面处加速度的放大效应刚好相反;加速度的放大效应具有一定的方向性,且该方向性与河岸两侧斜坡的坡度有关;加速度放大效应在河谷底部的分布具有不均匀性,距离河岸越近,加速度放大效应越强烈。 | 杨长卫 张建经 | 2013 | 岩石力学与工程学报2013，32，7： | 6 |
| 5 | Analysis on Dam-Breaking Mode of Tangjiashan Barrier Dam in Beichuan County显示文摘Tangjiashan landslide is a typical high-speed consequent landslide of medium-steep dip angle. This landslide triggered by earthquake took place in about semi-minute. The relative sliding displacement is 900 meters, so average sliding speed is about 30 meters per second. The longitudinal length of barrier dam which is formed by high-speed landslide along river is 803.4 meters; and maximum width crossing river is 611.8 meters. And its volume is estimated about 20.37 million steres. Through detailed geological investigation of the barrier dam, together with early geological information before earthquake, geological structures of the barrier dam and its stability of upstream and downstream slopes are studied when water level reaches different elevations in condition of continual after shocks with seismic intensity of 7 or 8 Richter scale. On this basis, dam-breaking mode of barrier dam is discussed deeply. Thereby, analytic results provide significant guidance and advices to front headquarters of Tangjiashan barrier dam, so that some proper engineering measures can be implemented and flood discharge can be carried out well. | HU Xiewen LUO Gang LV Xiaoping HUANG Runqiu SHI Yubin | 2011 | Journal of Mountain Science2011，8，2： | 6 |
| 6 | Numerical simulations of kinetic formation mechanism of Tangjiashan landslide显示文摘Tangjiashan landslide is a typical high-speed landslide hosted on consequent bedding rock.The landslide was induced by Wenchuan earthquake at a medium-steep hill slope.The occurrence of Tangjiashan landslide was basically controlled by the tectonic structure,topography,stratum lithology,slope structure,seismic waves,and strike of river.Among various factors,the seismic loading with great intensity and long duration was dominant.The landslide initiation exhibited the local amplification effect of seismic waves at the rear of the slope,the dislocation effect on the fault,and the shear failure differentiating effect on the regions between the soft and the hard layers.Based on field investigations and with the employment of the distinct element numerical simulation program UDEC(universal distinct element code),the whole kinetic sliding process of Tangjiashan landslide was represented and the formation mechanism of the consequent rock landslide under seismic loading was studied.The results are helpful for understanding seismic dynamic responses of consequent bedding rock slopes,where the slope stability could be governed by earthquakes. | Gang Luo Xiewen Hu Chengzhuang Gu Ying Wang | 2012 | Journal of Rock Mechanics and Geotechnical Engineering2012，4，2： | 3 |
| 7 | Slope Reinforcement for Housing in Three Gorges Reservoir Area显示文摘The Three Gorges Project of the Yangtze River is the largest hydropower-complex project under construction in the world. Under the largescale relocation projects, 2874 engineered slopes are formed along with the construction of new towns. In this paper, the cutting slopes are mainly soil slopes and rock slopes. Soil slopes include residual soil slopes, colluvial accumulation slopes, swelling soil slopes, and artificial earth fill slopes, etc. Rock slopes include blocky structure rock slopes, layer structure rock slopes, and clastic structure rock slopes, etc. Varied protection measures have been used for slope protection in the reservoir area including shotcrete concrete-anchor bars, frame beams, retaining walls, slope stabilizing piles, sheet-pile walls, anchorage anti-shear tunnels, flexible protection grids, and drainage, etc. Besides, slope deformation monitoring systems have been set up to monitor deformation failure and the stability state of slopes. The protection measures have guaranteed slope safety and maintained a harmony with the urban environment and surrounding landscape. | WU Faquan LUO Yuanhua CHANG Zhonghua | 2011 | Journal of Mountain Science2011，8，2： | 1 |
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