摘要
计算分析了枯木A滑坡在布设排水孔等工程处理措施前后,滑坡体的流网变化情况及排水措施的效果;计算了在强降雨和水库蓄水2种情况下,设置排水措施前、后滑坡堆积体各分区的平均含水率等指标情况,分析了强降雨对计算结果的影响。计算结果表明,排水措施对降低滑坡体的饱和度和含水量是有一定效果的;相对强降雨而言,水库蓄水对滑坡体的影响更大。
Variatian of the seepage network of the landslide mass and effect of the drainage facilities befiJre and after such the engineering facilities as,provision of drainage holes in the Landslide A at Kumu are calculated and studied. In conditions of strong rainfall and reser- voir impoundment, the average moisture contents of zones of the landslide before and 'after drainage holes are provided are calculated. Af- tbets on the calculation'results by the strong rainfall are analyzed. The calculation and analysis results prove that the drainage facilities de- crease properly saturation and moisture content of the landslide mass. Compared with affect by the strong rainfall, the reservoir impound- ruent 'affects seriously the landslide.
出处
《西北水电》
2013年第4期27-31,共5页
Northwest Hydropower
关键词
枯木A滑坡
非稳定渗流
排水措施
滑坡体稳定
鲁地拉水电站
Landslide A at Kumu
unstable seepage
drainage facility
landslide stability
Ludila Hydropower Project