XYZ
XYZ
1. Introduction ......................................................................................... 6
1.1 Project ................................................................................................................................................. 6
1.2 Organization of the Report .............................................................................................................. 7
2. References .......................................................................................... 7
5. Geotechnical Investigation............................................................... 11
5.1 Existing Information ........................................................................................................................ 11
5.1.1 Boreholes .................................................................................................................................. 11
5.1.2 Laboratory and Field Test ...................................................................................................... 16
6. Results ............................................................................................... 17
6.1 Laboratory Test Results ................................................................................................................. 17
6.1.1 Grain Size Distribution ............................................................................................................ 17
6.1.2 Natural Moisture Content ....................................................................................................... 17
6.1.3 Atterberg Limits ....................................................................................................................... 17
6.1.4 Bulk Density .............................................................................................................................. 18
6.1.5 Triaxial Testing ......................................................................................................................... 18
6.1.6 Chemical Aggressivity and Corrosion ................................................................................. 18
6.1.7 Tests on Rock........................................................................................................................... 18
6.2 Field Test Results ............................................................................................................................ 18
6.2.1 SPT ‘N’ Distribution .................................................................................................................. 18
6.2.2 Permeability Test Results ...................................................................................................... 19
7. Geotechnical Assessment ................................................................ 19
7.1 Soil Parameters ............................................................................................................................... 20
7.1.1 Consistency based on SPT Values ...................................................................................... 20
7.1.2 Bulk Density .............................................................................................................................. 20
7.1.3 Permeability .............................................................................................................................. 21
7.1.4 Strength and Stiffness Parameters ...................................................................................... 22
7.1.4.1 Undrained Behavior ............................................................................................................. 22
7.1.4.2 Drained Behavior ................................................................................................................. 23
7.2 Geotechnical Design Parameters for Soil ................................................................................... 24
7.3 Chemical Aggressivity and Corrosion – Soil and Groundwater .............................................. 24
7.4 Rock Parameters ............................................................................................................................. 25
7.4.1 Classification of Rock ............................................................................................................. 25
7.4.2 UCS Test Results of Rock ...................................................................................................... 27
7.4.3 Point Load Strength Index Test Results of Rock ............................................................... 27
7.4.4 Rock Mass Rating System (Bieniawski)................................................................................ 28
7.4.5 Geological Strength Index (GSI) ............................................................................................ 29
7.4.6 Deformation Modulus of Rock Mass .................................................................................... 31
7.4.7 Lugeon Test .............................................................................................................................. 31
Appendix – A ........................................................................................... 36
Plots for Soil ............................................................................................................................................. 36
A1. SPT vs Depth ..................................................................................................................................... 37
A2. Coefficient of permeability vs Depth ............................................................................................ 38
Appendix – B............................................................................................ 39
Plots for Rock ........................................................................................................................................... 39
B1. RQD vs Depth .................................................................................................................................... 40
B2. UCS of intact rock vs Depth ............................................................................................................ 41
B3. Point load index vs Depth ................................................................................................................ 42
B4. Elastic Modulus of intact rock vs Depth ....................................................................................... 43
B5. Coefficient of Permeability vs Depth ............................................................................................ 43
Appendix – C ........................................................................................... 44
Appendix – D ........................................................................................... 45
LIST OF FIGURES:
Figure 1: Map showing various Geological Units (after GSI……) ............................................................................. 10
Figure 2: Relationship between Φ and SPT N Value (IS: 6403 – 1981) ................................................................. 23
LIST OF TABLES:
Bangalore is the Information technology capital of India. Bangalore Metropolitan Region (BMR) is
one of the fastest growing regions in India. BMR is experiencing a rapid growth in population and
employment and this trend is expected to continue with immigrants from the hinterland of
Karnataka’s as well as from all parts of the Country attracted by job opportunities offered in
Bangalore.
In order to improve the overall traffic and transportation scenario in Bangalore and to cater the
future travel needs, the Government of Karnataka (GOK) through Bangalore Metro Rail Corporation
Limited (BMRCL) has undertaken several studies and identified metro model as efficient,
economically viable, secure and environment friendly mass transport system.
The DMRC submitted the DPR for Phase-I of the Namma Metro project to the BMRCL in May 2003,
but the final approval on a scheme come in April 2006. The DPR prepared by DMRC envisaged a
33 km (21 mi) elevated and underground rail network with 32 stations for Phase-I of the project. The
proposed gauge was standard gauge. The rationale for the metro includes reduced journey times,
cutting fuel use, accident reduction and lower pollution. Phase-I, Reach 1(east), Reach 2 (west),
Reach 3 & 3A (north), and reach 3B are operational, whereas Reach 4, 4A and UG1 Easts to West
and North to South will be opened soon.
Meanwhile, In 2011 The State Government appointed DMRC for carrying out detailed project report
(DPR) for Phase-II. The high power committee (HPC), in July 2011, gave in-principle clearance to
proceed with Phase-II. The Karnataka government gave in-principle approval to Phase II of the
Namma Metro project on 3 January 2012. Phase II was as well cleared by the expenditure finance
committee (EFC) in August 2013. The Union cabinet in 2014 approved plans for phase II.
Currently BMRCL has appointed Interim Design Consultants (IDC) for requisite services for the
preliminary designs /tender design and other related preparatory activities required for the purpose
of the Bidding for the Civil Works for the Red Line, Reach – 6 from Dairy Circle to Nagawara
underground stretch. IDC has also been asked to do the Detail design of M&E services for Reach 6.
BMRCL has appointed AECOM as Interim Design Consultant (IDC) for Civil, Architectural and E&M
Works of underground section and stations – total 13.070km and 12 underground stations, starting
from dairy Circle to Nagawara of Reach 6, for proposed Phase-II of BMRCL Project. The IDC carried
out site specific studies and has studied geotechnical data given by BMRCL.
1.1 Project
The Metro line (Phase-II) from Dairy circle to Nagawara Reach 6 corridor extends in South - North
direction for a stretch of 13.79 km, fully underground. The proposed stretch includes 12 stations.
The stations being:
Dairy Circle
MICO Industries
Vellara Road
M.G. Road
Shivaji Nagar
Cantonment
Pottery Town
Tannery Road
Venkateshapura
Arabic College
Nagawara
The construction of Bangalore Metro phase-II has been divided into four contract packages as
described in Table 1. This report has to be treated as a standalone GIR for Under Ground Civil
Contract Package T-104. The Geotechnical data available from the various investigations carried
out till date has been reviewed and analyzed to arrive at design parameters for Civil package T-104.
Package Description
BMR/PH-II/R6/UGC – 103 Dairy Circle Ramp at southern end of Vellara Road station
2. References
3. Project Information
From Dairy circle to Nagawara, the alignment follows south north direction for a stretch of 13.79
km. The entire alignment is divided into 4 packages as shown in Table 1.
The horizontal alignment with bore hole locations for package BMR/PH-II/R6/UGC – 104, is shown in
Appendix – C.
Table 2 : Underground Tentative Civil Contract Package T - 104 Alignment
Up line Length of
Package Chainage (m) Package Description
Start End (m)
The vertical rail alignment in Package T-104 passes through soil (silty sand/sandy silt) and rock
(granitic gneiss). The running tunnels within this package will get generally embedded in rock strata
of grade II, III and IV/V and partially in soil strata along the alignment. However at some locations,
tunneling will be in mixed ground i.e. soil/grade-II/III/IV/V rock is anticipated. The classification of
rock based on weathering grade is further detailed in section 7.4.1. The geological profile along the
alignment is shown in Appendix - C.
Geology wise, Bangalore district shows dominant presence of ‘Archaean’ crystalline rocks
comprising Peninsular Gneissic Complex with small patch of hornblende schist in the northern part
and intrusive Closepet granites all along the western part of the district. The gneissic rocks
are reported to be in the age range of 2.6 to 3.0 billion years. They are essentially grandioritic and
granitic in composition formed due to several tectono-thermal events with large influx of sialic
materials representing remobilized parts of an older crust with abundant additions of younger
granitic materials. The Peninsular Gneissic Complex constitutes the basement for schist belts that
are largely basaltic in composition and characterized by gold mineralization which is noticed in
Kolar Gold Fields located in adjacent Kolar district to the east of Bangalore distirict. Small stretches
comprising unconsolidated sediments are also noticed in Channapatna and Devanahalli.
The soil overburden generally is dominated by silty sand /residual silt and shows presence of clay
as a nominal interstitial binder. Overburden in upper layers is generally in loose /medium compact
condition especially in areas with high water table. The overburden thickness is variable and is
reflective of typical differential weathering that has occurred over a prolonged period. This is
followed by completely weathered rock and highly weathered rock. The geological map of
Bangalore district taken from Geological Survey of India (2000) and the same is presented in Figure
1.
Bangalore is situated at an altitude of about 900m above the mean sea level. It is located about
1150 kilometers south of tropic of cancer. The mean temperature varies from 170ºc to 380ºc. The
area has the benefit of northeast and southwest monsoons. The annual rainfall is about 760mm.
The weather is neither humid nor dry. The soil formation is due to physical weathering of parent
rock caused by temperature changes accompanied by chemical transformation.
4.2 Seismicity
Bangalore falls under Zone II of Seismic Zonation Map of India as per IS: 1893 (Part I) - 2002.
Recent earthquakes that occurred close to Bangalore were in the range of 2.0 to 5.5 on Richter
5. Geotechnical Investigation
Geotechnical Investigations have been carried out at various stages, a brief summary of which is
given below:
Station locations
5.1.1 Boreholes
Station
120 T(SN-CM)-6 782151.952 1436915.252 905.54 27 0 27
The following table shows a summary of field and laboratory tests done.
Table 5 : Existing Information: Field and Laboratory Testing
6. Results
This section contains the interpretation of test results and derivation of design parameters. The
geotechnical parameters described in the sections below are derived based on available data from
the investigation reports.
The field/laboratory test results are analyzed to study the general characteristics of the sub
soil layers. This is discussed in Sections 6.1 and 6.2.
The range of geotechnical parameters is taken corresponding to the values obtained from
the laboratory test results. This is discussed in Section 6.2.
Design parameters for this package are based on the information available from lab test and
literature as described in the followings sections.
The grain size distribution along the alignment indicates predominantly silty sand. In some areas
clayey silt layers with low compressibility are also observed. Detailed summary of grain size
distribution results are provided in the Geotechnical investigation reports.
Vast majority of samples scheduled for Atterberg Limits were deemed to be “Low to High Plastic”.
Plasticity Index values range from approximately 5% to 39% and Liquid Limit generally ranges from
25% to 70% indicating the material to be mainly sandy silt & clayey silt with low to high plasticity.
The bulk density for sandy silt / silty sand varies between 17.0 to 20.5 kN/m3 based on laboratory
test results. Since the values depend on degree of disturbance, the values are compared with the
range available in literature and appropriate values are picked for specific type of soil. The bulk
densities of the soil layers are taken in accordance with BS 8002:1994. This is discussed in section
7.1.2.
Triaxial tests were conducted on cohesive soil samples. However, the results were not consistent
and hence have not been used for deriving the design parameters. The strength parameters are
adopted based on empirical correlations with SPT ‘N’ values. This is discussed in Section 6.2.
Design of underground structures will be carried out in accordance with relevant Standards on
resistance to attack by ingress of sulphate and chloride.
Chemical analyses of soil-water extracted samples indicate that the pH value of water is in the
range of 4.16 to 8.48, sulphate content is in the range of (0.001 to 0.025 % by mass) 10 to 250 mg/l
and chloride content is in the range of (0.0016 to 0.058% by mass) 16 to 580 mg/l. The soil and
ground water is observed to be non-aggressive based on the lab test results. This is discussed in
Section 7.3.
The rock type encountered is mostly granitic gneiss along the alignment. Plots of RQD vs depth and
UCS of intact rock vs depth for all the rock samples are presented in
Appendix – B.
6.2 Field Test Results
Charts given in the Appendix – A show the distribution of field (uncorrected) SPT ‘N’ value with
depth for the soil types encountered along the specific stretches of the alignment. As per the plot,
2 to 4m of soil below ground level has SPT ‘N’ value ranging from 15 to 20. Below this depth, the
average SPT ‘N’ values increase with depth until refusal (>100) is observed on top of rock.
According to CIRIA Report 143 Table-9, as produced below, SPT values corrected to overburden
(N1) and 60% (N60) of theoretical free-fall hammer energy is used in determining the drained friction
angle of sands. In order to determine undrained cohesion, Elastic modulus of cohesive soils and
drained elastic modulus of granular soils, SPT values corrected to 60% of theoretical free-fall
Overburden correction factor can be calculated by using graph presented in CIRIA Report 143 (Fig.
28) and IS 2131 (Fig.1). Overburden correction factor is only required for deriving effective friction
angle (CIRIA 143) for cohesion less soils.
Field permeability tests were carried out to determine the permeability of soil. Based on the field
test results average permeability values for the different soil layers are summarized in the Table 7
below and the plot of test results with depth is presented in Appendix-A.
Table 7 : Permeability values for soil layers based on Test Results
7. Geotechnical Assessment
Laboratory test results are interpreted in Section 6.1 and 6.2. Accordingly the parameters for
different layers are aimed to be derived, based on the lab test results. However, the results are
found to be inconsistent and also there is lack of data at deeper depths. Therefore, the parameters
are derived from the SPT ‘N’ values based on empirical relationships. Interpretation of these
parameters is discussed in this section.
CIRIA Report recommends the procedure for determining the consistency of soil based on SPT ‘N’
values. The Chart given by CIRIA Report (Table-8) is reproduced below.
SPT N Values
SPT (N1)60 Values Consistency
(Uncorrected)
For Cohesion less Soils
0-4 0-3 Very loose
4-10 3-8 Loose
10-30 8-25 Medium
30-50 25-42 Dense
>50 >42 Very Dense
For Cohesive Soils
0-4 - Very Soft
4-8 - Soft
8-15 - Firm
15-30 - Stiff
30-60 - Very Stiff
>60 - Hard
The bulk densities of the soil layers are taken in accordance with BS 8002:1994 (Table-1).
Granular Soils
Gravel 16 18 20 21
Slag fill 12 15 18 20
Cohesive Soils
Organic Clay 15 15
Soft Clay 17 17
Firm Clay 18 18
Stiff Clay 19 19
Hard Clay 20 20
7.1.3 Permeability
In places where field/lab permeability tests are not available, it is possible to estimate approximate
values of “coefficient of permeability “ for soils as published in the FHWA manual, which is
reproduced below for easy reference.
Coefficient of
Drainage Soil Type
Permeability (cm/sec)
The soil that exhibits undrained behavior during excavation is assumed to have low permeability.
Clay and silt fall in this category.
Undrained shear strength (Cu) values is conservatively estimated, based on corrected SPT values
(N60) as per CIRIA Report 143.
Cu=5*N60 (kPa).............................................................................................Eqn 1
The same are also reflected in other references as given in Table 11 below where Undrained Shear
Strength is Cu=0.5*qu. The value of qu is approximately qu =12*N60.
Table 11 : Relationship between compressive strength and SPT Value and consistency of
saturated Cohesive Soils (from Terzaghi & Peck, 1967)
Undrained secant (elastic) modulus Eu is assumed to be based on corrected SPT value Correlation
as given below.
Eu=1.2*N60 (MPa)..............................................................Eqn 2 (CIRIA Report 143)
The undrained Poisson’s Ratio (μu) for total stress analysis is 0.5. In finite element analysis the value
to be used is 0.495 to avoid numerical instability. Values of Poisson’s ratio can be obtained from the
table below:
Silt 0.3-0.35
Rock 0.1-0.4
The coefficient of earth pressure at rest K o is estimated using the equation Ko= (1-sinφ’)
For Clayey and Silty Sand, the value of friction angle obtained from Figure 5 is reduced
by 5 degrees (IS 6403:1981).
The effective Poisson’s ratio μ’ is assumed to be 0.3 (from
Table 12).
The drained modulus E’ is computed based on correlation given in CIRIA Report 143.
For Clayey and Silty sand, E’ = 1.0*N60…………………………………Eqn 3
For Silt and Clay of medium to High Compressibility, E’ = 0.7*N60…..Eqn 4
The generalized values of design parameters for a particular type and consistency of soil/rock
encountered along the alignment are described in the following sections.
Geotechnical Design parameters are summarized in section 8.4. Values of SPT (N1)60 are only used
to calculate effective angle of internal friction for cohesion less soils.
Design of underground structures will be carried out in accordance with relevant Standards on
resistance to attack by ingress of sulphate and chloride.
The test results available to estimate the chemical aggressiveness of ground water and soil
indicate that both the soil and ground water are non-aggressive in nature.
Allowable limits of Chemical analysis of water are summarized in Table 13 to Table 15. In the current
case pH ranges from neutral to moderately alkaline. Chloride content is observed to be negligible
and sulphate content also falls under Class 1 which is considered negligible. Hence the soil and
ground water is generally non-aggressive in nature and no special care will be needed to prevent
corrosion. The table below shows the different categories of corrosiveness of chlorides and
sulphates in soil and ground water on concrete, as given in IS: 456.
Table 13 : Classification based on Sulphates in soil and ground water as per IS: 456
3 0.5 to 1 1200-2500
4 1 to 2 2500-5000
5 >2 >5000
Chloride Limits
Classification
Temperate Climate Tropical Climate
Very High Generally not applicable If only considerably in excess of 20,000 ppm
Classification pH
Extremely acid < 4.5
The soil and ground water are not aggressive as indicated by the chemical analyses. Hence no
special care needs to be taken for concrete.
Based on the Geotechnical assessment, Contract package T-104 has overburden soil followed by
rock. The rock type encountered along the stretch is predominantly Granitic Gneiss.
Classification of rock based on weathering grades is suggested in IS 4464. This is based on visual
observation of weathering of the rock and is more qualitative. The classification of rock based on
weathering grades (IS 4464) is presented in Table 16.
Table 16 : Classification of rock based on weathering grades (IS 4464)
Residual soil (VI) Friable soil with original rock fabric Extremely low
completely destroyed
Since the above classification system is qualitative, it was thought of bringing in a quantitative
approach to classification. In Chennai Metro, to have a quantitative approach to the classification,
Core Recovery (CR) and Rock Quality Designation (RQD) were introduced. For the Mumbai Metro
Line 3 a similar classification was adopted. Table 17 below shows the classification of weathering
grades followed in Chennai and Mumbai Metros.
Table 17 : Classification of weathering grades based on CR and RQD
Index Properties
Weathering class Description of rock Effective
Strength CR RQD
and grade material and rock Mass Porosity
[%] [%]
Considering the variability of the rock types, the weathering grades, the structural patterns like
jointing and foliations, and the strength of the intact rock along the alignment it was decided to
have a site specific classification system based on RQD alone. It may be noted that the geology of
Bangalore is far more complex and varied compared to Chennai or Mumbai.
The rock classification suggested for Bangalore Metro Reach 6 is given in Table 18. And a plot of
RQD vs Depth for rock strata is given in
Appendix – B.
Table 18 : Classification of weathering grades based on RQD
The unconfined compressive strength test was carried out on selected rock core samples. A plot of
the UCS of intact rock vs Depth for rock based on weathering grade is given in
Appendix – B.
Average UCS values are summarized in Table 19 below.
1 II 75
2 T-104 Granitic Gneiss III 60
3 IV/V 30
Point load tests were carried out on select intact rock core samples as per IS 8764. Although the
point load test is an index test for rock, it has been equated with the unconfined uniaxial
compressive strength. The Uniaxial compressive strength of rock predicted from the following
equation as given in IS 8764.
UCS = 22*Is(50)………………………………………………………………………...Eqn 5
Where,
Is(50) is corrected point load strength.
The average Is(50) values are presented in
Table 20
1 II 2 44.0
2 III 1.7 37.4
3 IV/V 1.2 26.4
The average UCS values obtained from Laboratory test results are compared with the empirically
calculated UCS values from Point Load Strength Index for Rock. Since higher values are observed,
no correlation between the two tests is established. Plots of the (Is) vs Depth are given in
Appendix – B.
7.4.4 Rock Mass Rating System (Bieniawski)
The Geomechanics classification or the Rock Mass Rating (RMR) system was initially developed at
the South African Council of Scientific and Industrial Research by Bieniawski (1973) on the basis of
his experience in shallow tunnels. This was further revised in 1989. The classification parameters
and ratings are reproduced in Appendix-D. IS:13365-(Part1)-1998 and further amended in 2008
gives guidelines for estimation of RMR.
For this project, the RMR classification has been carried out purely based on visual inspection of
available corelogs. Hence the parameters confirming discontinuities i.e. spacing, condition and
orientation are based on the reference given in Appendix-D and engineering judgement. This may
vary during the actual excavation of the tunnel.
RMR values and its correlation with the weathering grades are presented in the Table 21.
Separation
<1mm slightly
Grade II 75 7 >60 13 0.6-2 15 25 Damp 10 Unfavorable -10 60 III Fair Rock
weathered
walls
Separation
<1mm Highly
Grade III 60 7 30-60 8 0.2 - 0.6 10 20 Wet 7 Unfavorable -10 42 III Fair Rock
weathered
walls
Separation 1-
Very Poor
Grade IV/V 30 4 <30 3 <0.06 5 5 mm 10 Dipping 4 Unfavorable -10 16 V
Rock
continuous
Hoek and Brown (1997) introduced the Geological Strength Index (GSI), both for hard and weak rock masses. GSI value is derived from a chart that
classifies rock mass on the basis of visual inspection of geological condition presented in Table 22. This classification is incorporated in IS:13365 (Part 4)
which is in draft stage.
Table 22 : Representative values of GSI for different rock grade (IS 13365 Part 4)
GSI value is also calculated based on following equation provided by Bieniawski (1989).
GSI = RMR-5…………………………………………………………………………...Eqn 6
The GSI values for the rock mass are presented in Table 23.
IV/V 16 11
An estimation of deformation modulus (E m) of the rock mass can be obtained using GSI using the
relationship published by Hoek (2002).
………………………Eqn 7
Where,
D is disturbance factor (D=0, for TBM as described in the paper. D is also defined in IS 13365
(Part 4)
σci is Uniaxial Compressive Strength of intact rock, MPa
GSI is Geological Strength Index
The Deformation Modulus of rock mass for the different grades derived from Eqn 7 is presented in
Table 24.
Deformation Modulus, Em
Rock Class Rock Type σci, MPa GSI
(Hoek), GPa
II 75 55 11.55
Granitic
III 60 37 3.67
Gneiss
IV/V 30 11 0.58
Elastic modulii of intact rock obtained from lab test are also presented in Appendix-B.
Packer test also known as Lugeon test is a water pressure test, where a section of the drill hole is
isolated and water is pumped into that section until the flow rate is constant. Single packer
permeability tests are used in this project. A Lugeon is defined as the water loss of 1
liter/minute/length of test section at an effective pressure of 1 MPa. 1 Lugeon is approximately
equal to 10-7 m/s.
Water level observations during drilling of boreholes in the GI indicate ground water table ranging
from 10 to 16m depth below the ground level along the alignment except at shivajinagar station
where water level found to be at 6m below ground level.
In order to provide information on the seasonal variation, during construction phase, monitoring
shall be carried out in standpipe/piezometer installed at the shaft and station locations. It is
recommended to maintain water level monitoring installations during the site construction
activities.
Geotechnical assessment along the alignment is carried out in above sections. This stretch has soil
followed by rock strata at few locations continuous soil is encountered up to termination depth.
The soil deposit is predominantly silty sand & sandy silt of low plasticity. For the soil type in the
stretch, the available data indicate that the strength and stiffness parameters can be correlated to
SPT ‘N’ blow count.
The rock type is predominantly granitic gneiss observed throughout the stretch.
As per the available ground investigation results, the running tunnel within this package will
generally be embedded in rock of Grade III or higher with anticipated minimum rock cover of about
1.3m. At some locations, tunneling in mixed ground to soft ground is anticipated. This has to be
considered while calculating the volume loss and settlement prediction.
8.4 Design Parameters
Design parameters for soil and rock are derived from the plots presented in Appendix 1 and 2. Codes do not specify any guideline for the derivation of
design parameters, while it emphasizes on engineering judgement.
Table 26 : Generalized Design Parameters for Soil
line (N60)
Values
Detailed Parameters Parameters Parameters Parameters
Location
Description
cu u Eu c’ * ’ ^E’
μu μ'
kPa deg MPa kPa deg MPa
Vellara Road station Sandy SILT N = 18 + 5z (4<z<18) 18-88 - - - - 10 31-38 18-88 0.3
Tunnel between Vellara road
Sandy SILT N = 20 + 5z (4<z<12) 20-60 - - - - 10 32-36 20-60 0.3
and MG road stations
Sandy SILT
MG Road station N =12 + 4z (5<z<18) 12-64 - - - - 10 28-36 12-64 0.3
Table 26 summarizes the generalized design parameters for soil, for design of geotechnical works.
This is based on explanations provided in the previous section.
Deformatio
Rock Class
Rock Type
Rock, MPa
n Modulus
Lugeon
Em, GPa
UCS of
Grade
Intact
value
RMR
GSI
i ii iii iv v vi vii viii
II 75 60 III 55 0.5 11.55
Granitic
III Gneiss 60 42 III 37 1.5 3.67
It shall be noted that all design parameters are derived from the factual geotechnical data available
in 2014 with BMRCL as presented in Table 3 . Further, engineering judgement is exercised in
deriving the parameters. These parameters shall be cross verified by the contractor/DDC before
using them for detailed design.
Appendix – A
Plots for Soil
A1. SPT vs Depth
A2. Coefficient of permeability vs Depth
0 1 2 3 4 5 6
0
4
Depth (m)
10
12
14
Appendix – B
Plots for Rock
B1. RQD vs Depth
B2. UCS of intact rock vs Depth
B3. Point load index vs Depth
B4. Elastic Modulus of intact rock vs Depth
8
Depth (m)
12
16
20
24
28
32
Appendix – C
Geological Plan & Profile
Appendix – D
Geomechanics Classification (Rock Mass Rating)