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Investigation for the initiation of a loess landslide based on the unsaturated permeability and strength theory

机译:基于非饱和渗透率和强度理论的黄土滑坡萌生研究

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Background The Yanlian landslide, occurring on 21-22 October 2010, destroyed many facilities of a big oil refinery in Shaan’xi Province, China. It led to a suspending of the refinery work for a week and caused near 700 million RMB economic losses. Results Site exploration shows that the sliding mass is unsaturated-saturated loess. The groundwater is rich in the landslide and shortage in the surrounding slopes. Further investigation finds that the water drop released from the vapor heating furnaces on the top of the slope is the only source of the groundwater. Laboratory tests were performed to get the unsaturated strength parameters and hydraulic conductivity of the loess layers which were applied to a pre-failure slope model to simulate the water infiltration process and the stress field based on which the factor of safety is figured out to analyze the slope stability. Analysis shows that during the first ten years, the factor of safety has no prominent decrease. In the following 5?years, the slope stability decreases significantly till failure. Conclusions A little water infiltration has minor effects on slope stability for some time. As a result it is easy to be ignored. However, when the period of water infiltration is long enough to raise the groundwater level, it will have detrimental influence on the stability. In conclusion, any minor water produced by engineering or other activities for a long period may have harmful effect on slope stability. Therefore it is essential to take account of this kind of water and adopt measures to curb the surface water infiltration and to drain the groundwater.
机译:背景信息延边滑坡发生在2010年10月21日至22日,摧毁了中国陕西省一家大型炼油厂的许多设施。炼油厂停工一周,经济损失近7亿元。结果现场勘查表明,滑动体为不饱和饱和黄土。地下水富含滑坡,周围斜坡不足。进一步调查发现,从斜坡顶部的蒸气加热炉释放的水滴是唯一的地下水源。进行了室内试验,获得了黄土层的不饱和强度参数和水力传导率,将其应用到破坏前的边坡模型中,以模拟水的渗透过程和应力场,并据此找出安全系数来分析水土流失。边坡稳定性。分析表明,在最初的十年中,安全系数没有显着下降。在接下来的5年中,直到破坏,边坡稳定性显着下降。结论少量的水渗透对边坡稳定性影响较小。结果,很容易被忽略。但是,当渗水时间足够长以提高地下水位时,会对稳定性产生不利影响。总之,长期通过工程或其他活动产生的少量水可能会对边坡稳定性产生有害影响。因此,必须考虑到这种水并采取措施来抑制地表水的渗透并排干地下水。

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