首页> 外文期刊>International Journal of Geo-Engineering >Landslide hazard zonation mapping and cut slope stability analyses along Yercaud ghat road (Kuppanur–Yercaud) section, Tamil Nadu, India
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Landslide hazard zonation mapping and cut slope stability analyses along Yercaud ghat road (Kuppanur–Yercaud) section, Tamil Nadu, India

机译:印度泰米尔纳德邦Yarcaud ghat公路(Kuppanur–Yercaud)段的滑坡灾害分区图和边坡稳定性分析

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Abstract In the present study, the macro landslide hazard zonation (LHZ) mapping and slope stability analyses of selected rock slope (RS) sections were carried out along Kuppanur–Yercaud ghat road section. The macro LHZ map was prepared on 1:50,000 scale using landslide hazard evaluation factor (LHEF) rating scheme proposed by Bureau of Indian Standard IS 14496 (Part-2) 1998. The study incorporated predefined ratings for different causative factors viz. lithology, structure, slope morphometry, relative relief, land use and land cover, and hydrogeological condition as well as triggering factors like seismicity and rainfall. The total estimated hazard (TEHD) was evaluated by adding ratings of all the causative factors. On the basis of TEHD values, the facet 3 with TEHD value 6.25 was classified as high hazard zone (HHZ). The facet 2 and 4 with TEHD values 5.50 and 5.40 respectively was classified as moderate hazard zones (MHZ). The facet 1 and 5 with TEHD values 2.20 and 3.15 was categorized as very low hazard zone (VLHZ). The slope stability analyses were carried out in six RS sections using rock mass rating (RMR) and slope mass rating (SMR) systems and the factor of safety (FOS) was evaluated for critical discontinuity sets. The results of RMR show that RS sections?1, 2, 4, 5, and 6 fall in class-III fair rock category, whereas the RS section?3 falls in class-IV poor rock category. The SMR method involves field measurement of slope and discontinuity orientation. These structural values were plotted in the stereonet and identified possible direction and mode of failure. The results of SMR show that the rock sections?1, 2, 4, 5, and 6 falls under partially stable condition, while the rock section?3 comes under unstable condition. The FOS of the critical discontinuity sections was evaluated for planar as well as wedge failure modes. The results based on planar failure analysis, the RS-2 and RS-3 having FOS??1 are more unstable for slope failure. The wedge failure analysis shows that all the RS sections having FOS??1 fall in safe conditions.
机译:摘要在本研究中,沿着库普潘努尔-耶考德高止山脉路段,对选定的岩石边坡(RS)段进行了宏观滑坡灾害分区(LHZ)绘图和边坡稳定性分析。使用印度标准局IS 14496(第2部分)1998年提出的滑坡灾害评估因子(LHEF)分级方案,以1:50,000比例编制了宏观LHZ地图。该研究纳入了不同因果因子的预定义分级。岩性,结构,坡度形态,相对起伏,土地利用和土地覆盖以及水文地质条件以及诸如地震和降雨等触发因素。通过添加所有致病因素的等级来评估总估计危害(TEHD)。根据TEHD值,将TEHD值为6.25的方面3划分为高危险区(HHZ)。 TEHD值分别为5.50和5.40的小平面2和4被分类为中度危险区(MHZ)。 TEHD值分别为2.20和3.15的方面1和5被归类为极低危险区(VLHZ)。使用岩石质量等级(RMR)和斜坡质量等级(SMR)系统在六个RS段中进行了边坡稳定性分析,并评估了关键不连续性集的安全系数(FOS)。 RMR的结果表明,RS剖面?1、2、4、5和6属于III类中坚岩石类别,而RS剖面?3属于IV类中劣岩石类别。 SMR方法涉及现场测量坡度和不连续性。将这些结构值绘制在立体图中,并确定可能的故障方向和模式。 SMR的结果表明,岩石部分1、2、4、5和6处于部分稳定状态,而岩石部分3处于不稳定状态。对关键不连续部分的FOS进行了平面破坏模式和楔形破坏模式的评估。根据平面破坏分析的结果,FOS≤<1的RS-2和RS-3对于边坡破坏更不稳定。楔形破坏分析表明,所有FOS≥> 1的RS段都处于安全状态。

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