Physical Properties of Soil and Its Implication to Slope Stability of Nungbi Khunou , NH-150 , Manipur

Determination of physical property of the soil helps in identification and classification of soil which includes analysis of particle size distribution, Atterberg limits, water content, specific gravity, phase determination and direct shear test. Water plays an important role in triggering landslides and slope failures. Increase of water content reduces the stability of slope. When the moisture content exceeds plastic limits, the slope begins to deform. Three soil samples are collected from the study area and the average bulk density, moisture content and specific gravity are 1.577, 37.032 and 2.434 respectively. Atterberg limit is the most distinctive properties of fine grained sediments and may be used to distinguish silts from clays. Plastic limits (WP), liquid limit (WL), shrinkage limit (WS) values of Nungbi Khunou are 26.236%, 48% and 9.4% respectively. Plasticity index (IP), consistency index (IC) and liquidity index (IL) value is 21.764%, 0.379%, and 60.623% respectively. From index properties value, the soil is highly plastic, stiff and semi-solid in nature. The soil sample falls under CI group in plasticity chart which indicates organic silt and clay soil with medium compressibility and plasticity. Phase determination and particle size distribution result in very high porosity and highly saturated soils which are well graded in nature. Slope and aspect map are prepared from DEM using ArcGIS. Slope is an important contributory factor to landslide, and slope reported from the sampling area indicates gentle slope. Aspect refers to the direction of the terrain faces which is influenced by component like vegetation, settlement, agriculture, precipitation, wind etc. Factor of safety (Fs) calculated from shear stress data is less than 1 indicating unstable slope. From the above finding, the study area may result in sudden and unpredictable failure due to volumetric changes in soil. How to cite this paper: Bidyashwari, H., Kushwaha1, R.S., Chandra, M. and Okendro, M. (2017) Physical Properties of Soil and Its Implication to Slope Stability of Nungbi Khunou, NH-150, Manipur. International Journal of Geosciences, 8, 1332-1343. https://doi.org/10.4236/ijg.2017.811077 Received: August 10, 2017 Accepted: November 21, 2017 Published: November 24, 2017 Copyright © 2017 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY 4.0). http://creativecommons.org/licenses/by/4.0/


Introduction
Physical properties of soil, such as bulk density, cohesiveness and shear strength have been noted to affect stability of disturbed soil [1] [2] [3].Other authors [4] have also used similar properties to characterize the nature and behaviour of soils.Problem soil comprises of expansive, soft clay, collapsible and dispersive soil which may induce slope failure, due to their distinct shrink-swell properties at various moisture content [5] [6].Particle size and the distribution of pores within the soil matrix influence slope stability.Landslides are among the major hydro-geological hazards that affect large parts of the country.Northeast region, because of its fragile geological formation and structures, is highly prone to mass movement causing landslides.The major causes of the slides are both natural and anthropogenic.Geological formation along the road section between Ukhrul and Jessami along NH-150, belong to Disang and Barail groups.The constituent litho units are susceptible to weathering and erosion leading to slopes failure and mass wasting on moderate to large scale.The stratified nature of rocks, affected by deformation, plays an important role in causing landslides.No consideration of geological and geotechnical factors during construction considerably increases the incidences of landslides along the roads and hill slopes.Landslide hazard is defined as the probability of occurrence of landslides within a specific period of time and within a given area [7].

Geology of the Study Area
The present study area lies along national highway 150 between Ukhrul and Jessami (Figure 1).It is part of the mélange zone which belongs to the Indo-Myanmar Range (IMR).The study area is situated 38 km from Ukhrul town and belongs to Upper Disang Formation comprising rhythmic intercalation of fine grained sandstones, siltstones and shales (Plate 1(a)).Rocks are soft, fragile and highly weathered thereby converted to soil.The area is covered by a thick column of soil.Structural feature includes primary and secondary discontinuities in the rock such as bedding, foliation, joints, faults and fracture are very common in the nearby places.The sampling area has converted to terrace cultivated farm (Plate 1(b)) thereby leading instability of the slope.

Material and Method
In order to establish and characterize the problem nature of the slope material in terms of its implications for slope stability, a range of analysis were carried out at the geotechnical laboratory, Department of Earth Sciences, Manipur University.
The analysis focused on the distribution of soil particles, Atterberg limit and

Result of Soil Index Properties
The moisture content (W) is defined as the ratio of weight of water (W L ) to the weight of the soil solid (W d ) in a given mass of soil which is usually expressed as Measurement and recording of water content have done for those materials that were transported and stored in a sealed condition, providing confidence that the materials had not dried out between the time of sampling and testing in the laboratory.For the present work, oven drying method is used for determining the moisture content of soil sample.
The bulk density or the nature of in-situ weight of a soil in a unit volume, is expressed as where M = total mass of the soil, V = volume of the soil.
The bulk density is determined by using a core cutter and a weight balance.
Specific gravity of soil from the sliding zone is determined by using 50 ml density or specific gravity bottle.Data for moisture content, bulk density, specific gravity of the soil sample is shown in Table 1.
Three Phase determination of soil is important in identifying soil character.
Generally soil has three constituents which do not occupy separate space but are blend together forming a complex material.The interrelationships of the weights and volume of the three phases are important since they help in understanding the natural character of a soil.The volume of air (Va), water (Vw) and soil (Vs) are calculated from the measured index properties such as bulk density ( ρ ), specific gravity (G) and the natural moisture content (W).The total volume of the different element is assumed to be a unit volume.Volume relationship of three phases of soil from Nungbi Khunou Sample is shown in Table 2. Porosity, void ratio, degree of saturation, dry density and submerge density of the soil sample can be calculated from the values of three phases and is given in Table 3 below.

Soil Particle Distribution
Gradation curve for the representative soil sample of the study area is determined using both hydrometer and sieve methods.The results of the analysis are plotted to get a particle size distribution curve with the percentage finer N as the Ordinate and the particle diameter as the abscissa plotted on a logarithmic scale.
The particle size distribution curve gives us an idea about the type and gradation of the soil.A curve situated higher up or to the left represent a relatively fine grain soil while a curve situated to the right represent a coarse grain soil.A soil is said to be well graded when it has good representation of particles of all sizes.
On the other hand, a soil is said to be poorly graded if it has an excess of certain particles and deficiency of other or if it has most of the particles of about the  2) uniformity coefficient or coefficient of uniformity (C u ) is calculated, which is a measured of particle size range given by the ratio of D 60 and D 10 sizes.The shape of the particle size curve is represented by coefficient of the curvature C c given by ratio of square of D 30 the product of D 10 and D 60 : ( )

Atterberg Limits
Atterberg limits consistency limits means the relative ease with which soil can be deformed and denotes the degree of firmness of the soil.In order to determine the soil behaviour in respond to water content and its implication to landslide occurrence Atterberg limits were calculated and shown in Table 4.
Liquid limit of the study area is 48% indicating the high expansion potential of the soil.The moisture content of the soil is 37.032 which exceed the plastic limit of the soil.In this condition the deformation of the slope is possible and ultimately resulting the slope to an unstable condition.The plasticity index of a soil is commonly correlated with the expansion and residual angle of internal   friction for drained field condition [9].The greater the plasticity index, the more likely the soil is to become unstable and plastic under field condition [10].The plasticity index of the site indicates highly plastic soil.The soil is classified as semi solid and stiff from its consistency and liquidity index value.
Plasticity chart is used to classified fine grains.Many properties of clay and silt can be correlated with the Atterberg limit by means of plasticity chart [11].In the plasticity chart the ordinate represent the plasticity index and the abscissa the corresponding liquid limit.The chart is divided into different region.The A-line divides inorganic clay from silt and organic soil.Plasticity chart for the soil sample (Figure 3) falls under CI group which indicate organic silt and clay soil with medium compressibility and plasticity.

Shear Strength and Factor of Safety (Fs)
Plots of shear strength versus normal stress were used to compute the angle of internal friction and cohesion which were then used to calculate the factor of safety of the slope.Generally landslides occur when the disturbing/driving force (FD), which is chiefly resulted from the self-weight of the slope forming materials exceeds the resisting force (FR) given by the shear strength of the materials.
So, the factor of safety of a slope is the ratio of resisting forces to driving forces, i.e.F = resisting forces/driving forces.If the factor of safety is less than or equal to 1 (i.e., F ≤ 1), the slope will fail because driving forces will equal or exceed the resisting forces.If F is significantly greater than 1, the slope will be quite stable.Aspect refers to the direction to which a mountain slope faces which is generally express in term of degree from 0˚ to 360˚.Aspect is influence by component like vegetation, settlement, agriculture, precipitation, wind etc.The direction of the aspect was derived in 0˚ is true north; 90˚ aspect is to the east.The aspect map is shown in Figure 6.

Conclusion
The study area is part of Indo-Myanmar mobile belt and composed mainly of

H.Figure 1 .
Figure 1.Location map of the study area.
From the gradation curve the value of C u and C c is determined which indicates well graded sand with nearly 5% clay size particles.

Figure 2 .
Figure 2. Particle size distribution curve of soil sample.

Figure 3 .
Figure 3. Plasticity chart of the soil.

Figure 5 .
Figure 5. Slope map of the study area.

Disangshales,
Barail sandstone and Siltstone.Being a thrusting zone, rock of the region is highly deformed, jointed and prone to weathering.During heavy monsoon, soft lithology like shale and mudstone become mud and silt and susceptible to slide.This study determined the physical property of soil and its implica-H.Bidyashwari et al.DOI: 10.4236/ijg.2017.8110771342 International Journal of Geosciences

Figure 6 .
Figure 6.Aspect map of the study area.

Table 1 .
Physical parameters of the soil sample.

Table 2 .
Volume relationship of three phases of soil sample.

Table 3 .
Parameters derived from three phase analysis.International Journal of Geosciences same size it is known as uniformly graded soil.From the graph (Figure

Table 4 .
Data for Atterberg limits determination.