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库水位上升对古滑坡稳定性的影响
供稿: 宋丹青;​冯兴波 时间: 2018-11-12 次数:

作者:宋丹青冯兴波

作者单位:上海交通大学船舶海洋与建筑工程学院

摘要:以九甸峡库区坎前古滑坡为例,研究水库蓄水初期对古滑坡稳定性的影响。采用GPS对该边坡进行高精度、连续性的位移监测,结合滑坡具体的工程地质条件,对其变形特征进行分析,并且采用Geo-slope计算不同蓄水速率条件下的库岸边坡的安全系数。结果表明,蓄水初期库岸边坡整体较为稳定,蓄水速率越大对其稳定性越不利,库水上升速率超过0.5 m/d时将会发生局部失稳;滑体中部变形较大,变形速率具有逐渐变小的趋势;变形破坏模式为中后部分块、分级推移前缘的蠕变破坏特征。蓄水初期古滑坡整体较为稳定,库水位快速上升时将会出现局部失稳;采用Geo-slope分析滑坡稳定性变化规律,与采用GPS监测数据分析的规律相符,验证了监测数据的可靠性。

基金:国家重点基础研究发展计划(973计划)项目(2014CB744701); 国家自然科学基金资助项目(41401107);

关键词:库水位上升; 库岸边坡; 稳定性; GPS监测; 古滑坡;

DOI:10.16186/j.cnki.1673-9787.2016.06.021

分类号:P642.22

Abstract:Taking an example of an bank slope in Jiudian Gorge reservoir,the stability of ancient reservoir bank slope in early reservoir impoundment is studied. The displacement is used to preciously and continuously monitor by GPS,and the deformation characteristic of the slope was analyzed in combination with engineering geological conditions. The Geo-slope was used to calculate the stability of slope with rate of water level rise.The result shows that the stability of bank slope is stable on the whole,and the stability of landslide decreases with the water rising rate increasing,which the local instability will occour when it is more than 0. 5 m / d; the displacement of the middle part of the slope was the largest,the displacement velocity trended to become smaller generally; the displacement deformation model was creep damage characteristics which was the central block pull the leading edge. The stability of ancient landslide is stable generally,but the local slide occur.The analysis rule used by Geo-slope is in accordance with the law used by analyzing GPS data,which verifies that the monitoring data is reliable.

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