Abstract

The present paper deals with different empirical methods and finite element method of slope stability analysis along National Highway (NH)-7, in Uttarakhand, India. The highway is only path in the hilly terrain of Lesser Himalayan for the public transport and have strategic importance due to militaries possession routes. This route is also significant due to having many holistic places, connecting to this. There was numerous landslides happened along the Highway in past due to various natural and anthropogenic activities. Hence, keeping an eye to the socio-economic development of the distant area, slope stability analysis is very crucial along the road cut sections. To identify the vulnerable locations and to collect the geotechnical data, the field investigation was carried out between Shivpuri to Byasi along NH-7 in Garhwal, Uttarakhand. Then geotechnical data was intended followed by rock mass characteristic, kinematic analysis and Qslope stability. Additionally, to review the stability results, numerical simulation (finite element method) was employed and slope mass behavior and failure mechanism of cut slopes were also evaluated. The rock mass characteristic and kinematic analysis illustrate normal and good variety of rock mass mainly wedge mode with flexural toppling of failure. The slope mass rating, continuous slope mass rating and also Qslope stability analysis showed, road cut slopes are critically stable and unstable. The results of different empirical methods shows a decent correlation between them. Further the numerical simulation analysis also evaluates that two cut slopes are unstable and other one is critically stable. This substantial empirical and numerical analysis of cut slopes provides a collective approach to stable and develop the holistic road corridor in Himalayan terrain.

Highlights

  • Landslides in jointed rock slopes are one of the most incessant natural and anthropogenic hazards that have been frequently recorded in Himalayan terrain of the Uttarakhand region, India

  • This paper presents the rock mass characteristics (GSI and ­RMRbasic) and slope stability evaluation through empirical methods (SMR, Continuous slope mass rating (CoSMR) and ­Qslope stability) with kinematic analysis

  • Potential of flexural toppling (FT) failure at location L2 was prompted (Fig. 3). These predicted failures are mainly structurally controlled, where joint J­2 is critical joint set to initiate mass failure on cut slopes. ­RMRbasic was intended from five different rock-mass parameters based on recorded field and laboratory estimated data for all three locations

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Summary

Introduction

Landslides in jointed rock slopes are one of the most incessant natural and anthropogenic hazards that have been frequently recorded in Himalayan terrain of the Uttarakhand region, India. In Uttarakhand, RishikeshBadrinath (Mana) NH-7 is significant path for the transportation, public tourism and socio-economic activities. This mountainous road corridor is a prime medium for religious activity, where pilgrims use this route to reach their respective shrine and temples located in northern proximity of Uttarakhand. Increase in population imposes immense pressure on existing infrastructure of the Himalayan region and anthropogenic activity such as road development, tunnel and hydroelectric projects enhanced the frequency of occurrences of landslides in valley [24, 42, 43]. Percolation of water through weak fracture and joint plane exposed the overburden mass resting on the cut slopes and slip it down slope [53]

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