INTERNATIONAL JOURNAL OF LATEST TECHNOLOGY IN ENGINEERING,
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ISSN 2278-2540 | DOI: 10.51583/IJLTEMAS | Volume XIV, Issue III, March 2025
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Analysis of Road-Cut Slope in Calcareous Rocks and Stabilisation
by Shotcreting and Rock Bolting, Dehradun-Mussoorie Road,
Uttarakhand
Virat Singh Chauhan, Md. Rehan Sadique, Mohd. Masroor Alam
Aligarh Muslim University
DOI : https://doi.org/10.51583/IJLTEMAS.2025.140300033
Received: 01 April 2025; Accepted: 05 April 2025; Published: 14 April 2025
Abstract In this study, analysis and stabilisation of four road-cut slopes in the lesser Himalayan region near Mussoorie, along
Dehradun- Mussoorie Road, are investigated using the shotcreting and rock bolting technique. The rocks studied are calcareous in
nature with varying rock mass properties. The exposure is along the road cuts with slope varying from 70
0
to 90
0
, showing
toppling to wedge failure. The stability analysis is performed through the Finite Element Analysis (FEA) and Factor of Safety
(FOS) is evaluated using the Shear Strength Reduction Technique. The evaluation considers various conditions, including
unreinforced slopes and slopes reinforced with rock bolts and shotcrete, to thoroughly assess the effectiveness of rock bolting in
enhancing stability. The results indicate that rock bolting combined with shotcreting improves slope stability by approximately
1040% across the different slopes analyzed.
Keywords: Dehradun-Mussoorie Road, Limestone, Road-Cut Slope, FOS, Rock Bolting.
I. Introduction
Rock Bolts are one of the widely used methods of stabilisation in case of rocky slopes, tunnels, underground structure, mining
etc. The technique works by transferring load from the unstable slope surface to the interior stable slope with the help of high
yield strength deformed bars in combination with shotcreting (Hoek & Bray, 1981). This combination results in the increment in
the shear strength and overall stability of the rock mass (Hoek et al., 2000). Rock bolts are particularly effective in fractured or
jointed rock masses where they act by tying and reinforcing the jointed rock mass, thus reducing displacement, and preventing
failure (Singh and Goel 2011). The effectiveness of rock bolting largely depends on several factors such as the length, spacing,
orientation, and anchorage methods of the bolts, as well as the geological conditions of the slope (Singh and Goel 2011). The
geological condition of slope is governed by strength of rock and overall character of rock mass. The analysis of rock bolting can
be done by using Numerical Modelling techniques, such as the Finite Element Method (FEM) combined with the Shear Strength
Reduction (SSR) technique (Jing & Hudson, 2002) to evaluate the factor of safety of the slope.
The current study focuses on the stability analysis of four road-cut slopes along NH-707A near Mussoorie along Dehradun-
Mussoorie Road, Uttarakhand (Fig. 1a). The rocks are largely calcareous and include largely limestone with some dolomite
intercalations (Jiang et al.). The rock sequence stratigraphically belongs to Krol Formation, encircling the Mussoorie Syncline
(Fig. 1b). The rocks are moderately strong with less than 40 MPa of compressive strength. The rocks show loss of strength due to
random cracking at microscopic scale as well as due to weathering when dolomitised and comes down to 30 MPa. The roadside
view of the four locations is shown in Fig. 2.
(a)
INTERNATIONAL JOURNAL OF LATEST TECHNOLOGY IN ENGINEERING,
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(b)
Fig. 1: (a) Map showing the distribution of the various synclines within the Krol Belt which contains Tal Group (modified
after Jiang et al., 2002); (b) Geological Map showing Mussoorie location of the section examined (modified after Khan et al.,
2016).
The studied slopes are found to have slope varying from 70
0
to 90
0
(> 45
0
). The rock mass comprises three discontinuity sets with
varying spacing, forming rectangular to cuboid-shaped with volumes ranging from 0.08 to 0.2 at locations L1, L3, and L4.
Location L2 experiences wedge failure along three sets of conjugate joints, resulting in the formation of large prismatic wedges
with volumes ranging from 2 to 8 . While toppling failure is observed at locations L1, L3, and L4.
Fig. 2: Roadside view of the four road-cut slope locations.
The rocks are Micritic Limestones, moderately to highly weathered due to their presence in the humid tropical conditions. The
rocks show micro-fractures which are sealed with Calcite-Quartz veins (Fig. 3), suggestive of intense compressive tectonics
involved along the convergent plate margin, characteristic of Himalayan Tectonics.
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Fig. 3: Photomicrograph of Krol Limestone with Micro-Crystalline Calcite interspersed with micro veined cracks of calcite and
quartz. (a) Under Non-Polarised and (b) Under Polarized Light (60 X Magnification).
The analysis is performed on Rocscience RS2 software. The analysis is carried out in two stages: first, without reinforcement, and
then with reinforcement applied using shotcrete and rock bolting. The stability assessment is done to comprehensively evaluate
the effectiveness of rock bolting in enhancing the stability of the slope.
II. Method of Analysis
To carry out stability analysis in Rocscience RS2 software, the material parameters are collected from the field surveys and
laboratory studies for Slope Height, Slope Inclination, Geological Strength Index (GSI), rock mass characterization and
Unconfined Compressive Strength (UCS) of the rock material. The slope is modelled using six-node triangular elements. The
boundary condition is kept fixed at the bottom, while one side is restrained in one direction(Griffiths and Lane, 1999). The
geometry of the model with and without reinforcement is illustrated in Fig. 4. The material model is selected as Generalised
Hoek-Brown model due to the non -linear nature of the rock mass. The stability assessment is done using shear strength reduction
technique (Dawson et al., 1999). The material parameters utilised for slope stability analysis are shown in Table 1.
Table 1. Slope and Rock Mass Parameters used for performing Finite Element Analysis
Parameters
L1
L2
L3
L4
Height (m)
63
66
18
15
Inclination (°)
75
70
70
90
Unit weight (kN/m
3
)
27
27
27
27
UCS (MPa)
37
35
28
34
GSI
45
40
34
37
E
rm
(MPa)
2606
1834
837
1080
Bolt Length (m)
25
25
7
6
Fig. 4: (a) Geometry of the model for Location L1 without any reinforcement (b) Total Displacement profile for L1 (c) Geometry
with Shotcrete (d) Total Displacement with Shotcrete (e) Geometry with Shotcrete and Bolts (f) Total Displacement with
Shotcrete and bolts.
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III. Results and Discussion
The study focuses on the stability analysis of four road-cut slopes using Rocscience RS2 along Dehradun-Mussoorie Road. For
analyzing the slopes, Generalised Hoek Brown model is taken as material model. The stability analysis is performed using the
Shear Strength Reduction (SSR). The analysis is carried out in three stages, first without any reinforcement and second with
reinforcement as shotcrete and thirdly combination of shotcreting and rock bolts.
In the first stage, when no reinforcement is applied, the calculated FOS values for the four slopes were found to be 1.14, 1.05, and
0.72, 0.83 respectively. These low FOS values indicate marginal to unstable conditions of the slopes, which are caused due to
adverse orientation of discontinuities and slope, low Uniaxial Compressive Strength (UCS) of weathered limestone, Geological
Strength Index (GSI), steep slope angles and tectonic activity in this region.
In the second stage, shotcreting with a thickness of 20 cm is applied to the slope surfaces. The shotcreting resulted in a marginal
increase in FOS by 10-15%. While location L1 and L2 became stable with shotcreting, locations L3 and L4 remained in the
unstable category. In the subsequent stage, shotcreting is combined with rock bolts, with the bolts installed at a length equal to
40% of the slope height, diameter of 32mm, spacing 1.5m c/c and oriented at an inclination of 15° clockwise to the horizontal
plane. The inclusion of rock bolts significantly improves the stability of the slopes, with FOS values increasing by approximately
2040% as illustrated in Fig. 5. This improvement highlights the effectiveness of rock bolts in conjunction with shotcreting in
enhancing the slope stability by providing additional shear resistance and restricting potential failure mechanisms.
Fig. 5: Graph Showing Variation of Factor of Safety values for unreinforced and reinforced Slopes.
IV. Conclusions
This research employed Rocscience RS2 software through the Generalized Hoek-Brown model to determine stability aspects of
four road-cut slopes along NH-707A in Mussoorie, Dehradun, Uttarakhand India. Three different conditions were evaluated using
the Shear Strength Reduction method for determining the Factor of Safety (FOS): initially without reinforcement, with
shotcreting and with shotcreting combined with rock bolt installation. The analysis performed without rock bolts produced
stability results of 1.14, 1.05, and 0.72, 0.83 which indicated partial stable to unstable behaviour due to very unfavourable
discontinuity orientation, low UCS, GSI values along with steep slopes in a active tectonic setup.
The application of 20 cm thick shotcreting marginally improves FOS by 1015%, stabilizing locations L1 and L2 but leaving L3
and L4 in the unstable category. However, the combined application of rock bolts and shotcreting significantly enhances slope
stability. Rock bolts with lengths measuring 40% of slope height became more effective when installed at 15° inclination thus
raising the FOS by 2040%. The performance of rock bolts becomes apparent because they provide shear strength enhancement
which controls potential failure conditions. The study concludes that rock bolting is a practical stabilization technique for road-cut
slopes in challenging geo-tectonic conditions, such as in Himalayan states.
References
1. Hoek, E., & Bray, J. W. (1981). Rock Slope Engineering (3rd ed.). The Institution of Mining and Metallurgy, London.
2. Hoek, E., Carranza-Torres, C., & Corkum, B. (2000). Rock mass properties for underground mines. In Proceedings of
the North American Rock Mechanics Symposium.
3. Singh, B., & Goel, R. K. (2011). Engineering Rock Mass Classification: Tunnelling, Foundations and Landslides.
Elsevier.
0.6
0.7
0.8
0.9
1
1.1
1.2
1.3
1.4
1.5
1.6
1 2 3 4
Factor of Safety (FOS)
Locations (L1-L4)
No Reinforcement
Shotcrete
Shotcrete with Rock
Bolts
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4. Jing, L., & Hudson, J. A. (2002). Numerical methods in rock mechanics. International Journal of Rock Mechanics and
Mining Sciences, 39(4), 409427.
5. Griffiths, D. V., & Lane, P. A. (1999). Slope stability analysis by finite elements. Géotechnique, 49(3), 387403.
6. Dawson, E. M., Roth, W. H., & Drescher, A. (1999). Slope stability analysis by strength reduction. Géotechnique, 49(6),
835840.
7. Khan, K. F. and Israeli, S. H. (2005) Geochemistry and depositional environment of Mussoorie phosphorite deposits,
district Dehradun, Uttaranchal, India., J. Appl. Geochem., 7 (2) (2005), pp. 227-247.
8. Jiang, G., Christie-Blick, N., Kaufman, A.J., Banerjee, D. M. and Rai, V. (2002). Sequence Stratigraphy of the
Neoproterozoic Infra Krol Formation and Krol Group, Lesser Himalaya, India., J. Sediment. Res., 72 (2002), pp. 524-
542.
9. Khan, S. A., Dar, S. A., Khan K. F. and Karim, Y. (2022). Geochemical Characteristics of Early Cambrian Phosphate
Bearing Sedimentary Rocks from the Mussoorie Syncline, India: Implications for Paleo-Redox Conditions. Geosystems
and Geoenvironments, V 1 Issue 3., https://doi.org/10.1016/j.geogeo.2022.100046.