利用岩石科学滑动模型分析和减缓中巴经济走廊沿线(kkh)的边坡稳定性(以巴基斯坦humarri滑坡为例)

F. Javed, I. Khan
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引用次数: 0

摘要

巴基斯坦北部是地球上最活跃和最危险的地质地带之一。因此,历史上该地区发生过几次巨大的山体滑坡,破坏了基础设施,阻塞了罕萨河,严重破坏了喀喇昆仑公路。由于物流困难,距离遥远,尽管频繁发生大规模滑坡和随后的破坏,整个地区仍未得到充分研究。采用极限平衡法对巴基斯坦吉尔吉特上罕萨地区Humarri Nagar村罕萨河(HR)沿线的边坡破坏进行了研究。利用Slide Rocscience程序对该边坡进行了地质条件、边坡几何形状、土体强度参数和FOS测定等方面的研究。从斜坡上收集的土壤样本用于分析岩土力学特性,并在游览期间分析了斜坡的几何形状。土样的强度参数为含水率(w) 1%,比重(Gs) 2.64,单位重量(r) 19kN/m3,内摩擦角(AIF) 30,黏聚力(c) 69 kPa。统一分类系统(UCS)将Humarri活动滑坡土归类为砂质粉土,组号为ML。在Slide Rocscience程序中,使用LEM计算边坡的FOS,假设采用普通(O)、Janbu (J)和Bishop (B)技术。通过一组实例计算了孔隙水压力(PWP)、单位重量、黏聚力、内摩擦角和覆盖层对FOS的影响。随着黏结度和内摩擦角的增大,FOS增大;然而,FOS随着单位重量和上覆材料覆盖层的增加而增加。此外,虽然PWP有一些好的效果,但增加它会导致FOS显著下降。由于每个FOS都大于1,因此根据现有强度指标和模拟滑心结果判断Humarri活动滑坡在当前形态下是稳定的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SLOPE STABILITY ANALYSIS AND MITIGATION ALONG CPEC ROUTE (KKH) BY USING ROCSCIENCE SLIDE MODELING;(A CASE STUDY OF LANDSLIDE AT HUMARRI, PAKISTAN
Northern Pakistan is one of the most active and dangerous geological zones on the planet. As a result, several huge landslides have occurred in the area throughout history, destroying infrastructure, blocking the Hunza River, and seriously damaging the Karakoram highway. Due to the difficult logistics and wide distances involved, despite the high frequency of large-magnitude landslides and the subsequent destruction, the whole area remains understudied. Using the Limit Equilibrium Method, this study explores the slope failure along the Hunza River (HR), Village Humarri Nagar District Upper Hunza Gilgit Baltistan, Pakistan (LEM). Using Slide Rocscience programmer, the slope was fully studied for geological conditions, slope geometry, soil strength parameters, and FOS determination. Soil samples from the slope were gathered for analysis of geotechnical properties, and the slope's geometry was also analysed during the excursion. Moisture content (w) 1%, specific gravity (Gs) 2.64, unit weight (r) 19kN/m3, angle of internal friction (AIF) 30 and cohesion (c) 69 kPa are the strength parameters of the soil sample. The Humarri active landslide soil was classed as sandy silt with the group sign ML by the Unified Classification System (UCS). In Slide Rocscience programme, the FOS of the slope was calculated using LEM with the assumption of ordinary (O), Janbu (J), and Bishop (B) techniques. A set of instances were used to calculate the influence of Pore Water Pressure (PWP), Unit Weight, Cohesion, Angle of Internal Friction, and Overburden on FOS. FOS increases when cohesiveness and angle of internal friction rise; yet, FOS increases as unit weight and overburden of overlying materials grow. Furthermore, while PWP has some good effects, increasing it causes a significant decline in FOS. Because every FOS is larger than 1, the Humarri active landslide is judged to be stable in its current form based on available strength metrics and simulated slide conscience results.
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