Mitigation and management of rainfall induced rockslides along the national highways of Himalayan region, India

The research focuses on slope stability analysis and stabilization measures of Dhalli landslide, Himachal Pradesh. Kinematic analysis reveals joints J1 and J2 dip towards the bedding plane causes a wedge failure. Field investigation of the rock slope was conducted using Slope Mass Rating method (SMR...

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Main Authors: Prakasam C, Aravinth R, Varinder S Kanwar, B Nagarajan
Format: Article
Language:English
Published: Taylor & Francis Group 2021-01-01
Series:Geomatics, Natural Hazards & Risk
Subjects:
Online Access:http://dx.doi.org/10.1080/19475705.2021.1928772
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spelling doaj-d28ab7ac41e849a784573084ca0634922021-06-11T09:33:07ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132021-01-011211402142510.1080/19475705.2021.19287721928772Mitigation and management of rainfall induced rockslides along the national highways of Himalayan region, IndiaPrakasam C0Aravinth R1Varinder S Kanwar2B Nagarajan3Department of Civil Engineering, Chitkara UniversityDepartment of Civil Engineering, Chitkara UniversityDepartment of Civil Engineering, Chitkara UniversityNational Centre for Geodesy, Indian Institute of TechnologyThe research focuses on slope stability analysis and stabilization measures of Dhalli landslide, Himachal Pradesh. Kinematic analysis reveals joints J1 and J2 dip towards the bedding plane causes a wedge failure. Field investigation of the rock slope was conducted using Slope Mass Rating method (SMR) which asses the stability of slopes using a rating schemes of (0–100). The results revealed an SMR value of 45 indicating the slope is partially stable. The strength of the rock materials was estimated using ten core samples through point load test indicating an average failure load of 5.4 MPa revealing rocks are weak to moderately strong in nature. Based on the results from the field investigation and landslide morphometry slope stability of the rockslide has been calculated based on the Mohr–Columb failure criterion using Rocscience software. J1 and J2 has a combined wedge area of 1884 sq. m with an FOS value of 0.9 indicating that the slope is partially stable. A suitable stabilization method was proposed using reinforced wired net mesh with a grid spacing of 15 × 15 cm and shotcrete of 30 cm thickness with as FOS of 1.6 indicating the stability of the slope post-stabilization measure.http://dx.doi.org/10.1080/19475705.2021.1928772dhalli landslideslope stabilitykinematic analysisrainfall thresholdswedge
collection DOAJ
language English
format Article
sources DOAJ
author Prakasam C
Aravinth R
Varinder S Kanwar
B Nagarajan
spellingShingle Prakasam C
Aravinth R
Varinder S Kanwar
B Nagarajan
Mitigation and management of rainfall induced rockslides along the national highways of Himalayan region, India
Geomatics, Natural Hazards & Risk
dhalli landslide
slope stability
kinematic analysis
rainfall threshold
swedge
author_facet Prakasam C
Aravinth R
Varinder S Kanwar
B Nagarajan
author_sort Prakasam C
title Mitigation and management of rainfall induced rockslides along the national highways of Himalayan region, India
title_short Mitigation and management of rainfall induced rockslides along the national highways of Himalayan region, India
title_full Mitigation and management of rainfall induced rockslides along the national highways of Himalayan region, India
title_fullStr Mitigation and management of rainfall induced rockslides along the national highways of Himalayan region, India
title_full_unstemmed Mitigation and management of rainfall induced rockslides along the national highways of Himalayan region, India
title_sort mitigation and management of rainfall induced rockslides along the national highways of himalayan region, india
publisher Taylor & Francis Group
series Geomatics, Natural Hazards & Risk
issn 1947-5705
1947-5713
publishDate 2021-01-01
description The research focuses on slope stability analysis and stabilization measures of Dhalli landslide, Himachal Pradesh. Kinematic analysis reveals joints J1 and J2 dip towards the bedding plane causes a wedge failure. Field investigation of the rock slope was conducted using Slope Mass Rating method (SMR) which asses the stability of slopes using a rating schemes of (0–100). The results revealed an SMR value of 45 indicating the slope is partially stable. The strength of the rock materials was estimated using ten core samples through point load test indicating an average failure load of 5.4 MPa revealing rocks are weak to moderately strong in nature. Based on the results from the field investigation and landslide morphometry slope stability of the rockslide has been calculated based on the Mohr–Columb failure criterion using Rocscience software. J1 and J2 has a combined wedge area of 1884 sq. m with an FOS value of 0.9 indicating that the slope is partially stable. A suitable stabilization method was proposed using reinforced wired net mesh with a grid spacing of 15 × 15 cm and shotcrete of 30 cm thickness with as FOS of 1.6 indicating the stability of the slope post-stabilization measure.
topic dhalli landslide
slope stability
kinematic analysis
rainfall threshold
swedge
url http://dx.doi.org/10.1080/19475705.2021.1928772
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