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The quantitative classification system of rock mass - Guidelines, Part 1: RMR for predicting engineering properties

IS 13365 Part 1:1998 establishes a quantitative classification system known as Rock Mass Rating (RMR) for assessing rock masses to predict their engineering properties. This standard guides engineers in evaluating rock strength, discontinuities, groundwater conditions, and orientation to support design decisions in tunneling, slope stability, and foundation engineering. It is essential for geotechnical engineers, rock mechanics specialists, and civil engineers involved in underground and surface rock engineering projects.

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87Clauses Indexed
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1998Edition
Rock MechanicsCategory
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What This Standard Covers

IS 13365 Part 1:1998 establishes a quantitative classification system known as Rock Mass Rating (RMR) for assessing rock masses to predict their engineering properties. This standard guides engineers in evaluating rock strength, discontinuities, groundwater conditions, and orientation to support design decisions in tunneling, slope stability, and foundation engineering. It is essential for geotechnical engineers, rock mechanics specialists, and civil engineers involved in underground and surface rock engineering projects.

Who Uses This Standard

  • Geotechnical Engineers
  • Rock Mechanics Specialists
  • Civil Engineers
  • Mining Engineers
  • Tunnel Designers
  • Foundation Engineers
  • Geologists

Key Topics Covered

Rock Mass Rating (RMR) system
Uniaxial compressive strength and point load strength
Rock Quality Designation (RQD)
Spacing and condition of discontinuities
Groundwater conditions and their effect on rock mass
Orientation of discontinuities and joint favorability
Modulus of deformation correlations
Estimation of support pressure in tunnels
Stand-up time for unsupported spans
Adjustment factors for joint orientation
Prediction of tunneling ground conditions
Data collection and rating procedures
Use of empirical correlations for engineering properties

Table of Contents

1Scope

IS 13365 Part 1: Scope & Key Specifications

  • Scope:
    This standard provides guidelines for classification and characterization of rock masses for engineering purposes, focusing on rock mass quality, strength, and support design.

  • Key Parameters (Clause 3.1.1):

    • Uniaxial Compressive Strength (qc):
      Determined per IS 9143, IS 8764, or IS 10785 from rock cores. Preferred over point load strength.
    • Rock Mass Number (N):
      Used for predicting ground conditions:
      [ N = Q \times SRF ] where
      • ( Q ) = Rock Quality Designation
      • ( SRF ) = Stress Reduction Factor
  • Rock Mass Behavior Classification (Fig. 4):
    Based on ( N ), tunnel depth, and width, ground conditions are categorized as:

    • Self-supporting
    • Non-squeezing
    • Mild, Moderate, or High Squeezing
  • Referenced IS Codes (Annex A):

    IS No.Title
    8764:1978Point Load Strength Index of Rocks
    9143:1979Unconfined Compressive Strength of Rock Materials
    9221:1979Modulus of Elasticity and Poisson's Ratio of Rock
    11315 (Parts 1-3)Quantitative Description of Discontinuities

Summary Table: Rock Mass Number & Ground Condition

Rock Mass Number (N)Ground Condition
HighSelf-supporting
ModerateNon-squeezing
LowMild to High Squeezing

flowchart TD
    A[Rock Quality (Q)] --> C[Rock Mass Number (N)]
    B[Stress Reduction Factor (SRF)] --> C
    C --> D{Ground Condition}
    D -->|High N| E[Self-supporting]
    D -->|Moderate N| F[Non-squeezing]
    D -->|Low N| G[Mild to High Squeezing]

Note: Use latest editions of referenced IS codes for accurate

2References

IS 13365 Part 1 (1998) - Key References, Formulas & Tables


1. Rock Mass Number (N) and Ground Condition Prediction

  • Rock Mass Number:
    [ N = Q \times SRF ] where Q = Rock Quality, SRF = Stress Reduction Factor.

  • Tunneling Conditions (Clause 5.1.8 / Fig.4):

Ground ConditionCorrelation (H = Overburden, B = Tunnel Width, N = Rock Mass Number)
Self-supporting( H < 23.4 \times N^{0.89} \times B^{-0.1} ) and ( H < 1000 \times B^{-0.1} )
Non-squeezing( 23.4 \times N^{0.88} \times B^{-0.1} < H < 275 \times N^{0.33} \times B^{-0.1} )
Mild squeezing( 275 \times N^{0.33} \times B^{-0.1} < H < 450 \times N^{0.33} \times B^{-0.1} )
Moderate squeezing( 450 \times N^{0.33} \times B^{-0.1} < H < 630 \times N^{0.33} \times B^{-0.1} )
High squeezing( H > 630 \times N^{0.33} \times B^{-0.1} )

2. In-situ Modulus of Deformability (E in GPa)

  • Empirical correlations with Rock Mass Rating (RMR):

[ E = 2 \times RMR - 100 ] [ E = 10 \times \frac{(RMR - 10)}{40} ] [ E = 10 \text{ to } 40 \times \log_{10} Q ]


3. Recommended Indian Standards (Annex A)

IS No.Title
IS 8764:1978Point Load Strength Index of Rocks
3Collection of Field Data

IS 13365 Part 1: Collection of Field Data (Clause 3.1 & 3.1.1)

  • Key Parameter:

    • Uniaxial Compressive Strength (UCS), qc of intact rock cores is primary for rock strength assessment.
  • Testing Standards:

    • UCS tests on rock cores should follow:
      • IS 9143 (Rock core sampling)
      • IS 8764 (Methods of rock testing)
      • IS 10785 (Rock testing procedures)
    • Point Load Strength Index is secondary; UCS preferred.
  • Data Recording:

    • Use data sheet format as per Annex B of IS 13365 Part 1 for recording parameters including UCS and point load strength.
  • Rating System (Annex B, Item I):

    • Rock strength classification based on UCS values, e.g.:
      UCS (MPa)Rock Strength Rating
      > 250Very High
      100 – 250High
      50 – 100Medium
      < 50Low
  • Important Note:

    • Correlations using UCS are for feasibility and preliminary designs only.
    • In-situ tests (e.g., plate load, pressuremeter) are essential for final design.

Summary Diagram of Data Collection Flow

flowchart TD
    A[Rock Core Sampling] --> B[UCS Testing (IS 9143/8764/10785)]
    B --> C[Record UCS in Data Sheet (Annex B)]
    C --> D{Use for Design Stage?}
    D -->|Preliminary| E[Use UCS Correlations]
    D -->|Final| F[Conduct In-Situ Tests]

This ensures structured, reliable rock mass characterization per IS 13365 Part 1.

4Estimation of Rock Mass Rating (RMR)

IS 13365 Part 1: Key Formulas & Tables for Rock Mass Rating (RMR)


1. Rock Mass Rating (RMR) Overview

  • RMR classifies rock mass based on:
    • Uniaxial compressive strength of rock material
    • Rock quality designation (RQD)
    • Spacing of discontinuities
    • Condition of discontinuities
    • Groundwater conditions
    • Orientation of discontinuities (excluded if considered separately)
  • Used to predict engineering properties like support pressure, stand-up time, and modulus of deformability.

2. Estimation of In-Situ Modulus of Deformability (E)

Three empirical correlations (E in GPa):

Formula No.FormulaReference
(1)( E = 2 \times RMR - 100 )Bieniawski (1978)
(2)( E = 10 \times \frac{(RMR - 10)}{40} )Pereira (1983)
(3)( E = 10 \text{ to } 40 \times \log_{10} Q )Q = Rock Quality Index

3. Prediction of Tunnelling Conditions (Clause 23.4)

  • (N) = Rock mass number (from 4.3)
  • (H) = Overburden (m)
  • (B) = Tunnel width (m)
ConditionRange of H (m)Expression
No squeezing(H < 23.4)(N^{0.1} B^{-0.1})
Moderate squeezing(275 < H < 630)(N^{0.33} B^{-0.1})
High squeezing(H > 630)(A^{0.33} B^{-0.1})

Note: Avoid double counting pore water pressure or joint orientation in both RMR and stability analysis.


4. Rock Mass Quality Classification

| RMR Range | Rock Quality (Q) | Description | |-----------

5Engineering Properties of Rock Masses

Engineering Properties of Rock Masses (IS 13365 Part 1)

1. Rock Mass Rating (RMR) & Classification (Table 1)

RMR RangeClassRock Mass QualityAvg. Stand-up TimeCohesion (kg/cm²)Friction Angle (°)
100-81IVery Good10 years (15 m span)>4>45
80-61IIGood6 months (8 m span)3-435-45
60-41IIIFair1 week (5 m span)2-325-35
40-21IVPoor10 hours (2.5 m span)1-215-25
<20VVery Poor30 minutes (1 m span)<115

2. Shear Strength of Jointed Rock Masses (Clause 5.1.6)

  • For poor rock masses (RMR < 60):

    [ \tau = A(\sigma_n + T)^B, \quad \tau = 0 \text{ if } \sigma_n < 0 ]

  • For hard rock masses (RMR > 60):

    [ \tau_n = A(\sigma_n + T)^B, \quad \tau_n = 0 \text{ if } \sigma_n < 0 ]

Where:

  • (\tau) = shear strength
  • (\sigma_n) = normal stress on the joint
  • (A, T, B) = constants (from Table 2, varies with moisture and saturation)
  • (q_c) = uniaxial compressive strength of intact rock

3. Mobilised Uniaxial Compressive Strength for Tunnels:

[ q_{c, \text{mass}} = 70 \text{ MPa (approx.) for } Q \leq 10, J_w = 1

6Prediction of Tunneling Conditions

Prediction of Tunnelling Conditions (IS 13365 Part 1, Clause 5.1.8)

Tunnelling ground conditions are predicted using the correlation between Rock Mass Number (N), Tunnel Overburden (H in m), and Tunnel Width (B in m):

Ground ConditionCorrelation Range for H (m)
Self-supporting( H < 23.4 , N^{0.89} B^{-0.1} ) and ( 1000 , B^{-0.1} )
Non-squeezing( 23.4 , N^{0.88} B^{-0.1} < H < 275 , N^{0.33} B^{-0.1} )
Mild squeezing( 275 , N^{0.33} B^{-0.1} < H < 450 , N^{0.33} B^{-0.1} )
Moderate squeezing( 450 , N^{0.33} B^{-0.1} < H < 630 , N^{0.33} B^{-0.1} )
High squeezing( H > 630 , N^{0.33} B^{-0.1} )
  • N = Rock Mass Number (from IS 13365 Clause 4.3)
  • H = Overburden depth (m)
  • B = Tunnel width (m)

Additional Key Formulas:

  • In-situ Modulus of Deformability, E (GPa):

[ \begin{cases} E = 2 \times RMR - 100 \ E = 10 \times \frac{RMR - 10}{40} \ E = 10 \text{ to } 40 \times \log_{10} Q \end{cases} ]

  • Overburden vertical stress:

[ \sigma_v = 0.27 \times H \quad (\text{kg/cm}^2) ]


Notes:

  • Avoid double counting parameters in RMR and structural analysis (e.g., pore water pressure or joint orientation).
  • Groundwater inflow should be measured or qualit
7Estimation of Support Pressure

Estimation of Support Pressure (IS 13365 Part 1)

Key Formula (Clause 7.5):

[ \text{Proof} = \frac{7.5 \times B^{0.1} \times H^{0.5} - \text{RMR}}{2 \times \text{RMR}} \quad \text{(kg/cm}^2) ]

  • B = Span of opening (m)
  • H = Overburden/tunnel depth (m), typically > 50 m
  • RMR = Rock Mass Rating

Allowable Bearing Pressure

  • Related to RMR, estimated as per IS 12070 (refer IS 12070 for detailed tables).

Prediction of Tunnelling Conditions (Clause 5.1.8)

Ground ConditionCorrelation for Depth (H) (m) vs RMR (N) and Span (B) (m)
Self-supporting(H < 23.4 \times N^{0.89} \times B^{-0.1}) and (H < 1000 \times B^{-0.1})
Non-squeezing(23.4 \times N^{0.88} \times B^{-0.1} < H < 275 \times N^{0.33} \times B^{-0.1})
Mild squeezing(275 \times N^{0.33} \times B^{-0.1} < H < 450 \times N^{0.33} \times B^{-0.1})
Moderate squeezing(450 \times N^{0.33} \times B^{-0.1} < H < 630 \times N^{0.33} \times B^{-0.1})
High squeezing(H > 630 \times N^{0.33} \times B^{-0.1})

Notes:

  • Use Q-system (IS 13365 Part 2) with correct Stress Reduction Factor (SRF) for more reliable support pressure.
  • These empirical relations are for steel rib supports in conventional blasting tunnels.

flowchart TD
    A[Input: Span
8Stand-up Time for Unsupported Span

Stand-up Time for Unsupported Span
(IS 13365 Part 1:1998)


Key Definitions:

  • Effective Span = Minimum of (size of opening, distance between tunnel face & support)
  • For arched openings, stand-up time is significantly higher than flat roofs.
  • Controlled blasting increases stand-up time by reducing rock damage.

Stand-up Time Guidelines (Clause 2.5 & Fig.1):

Unsupported Span (m)Stand-up Time (hours)
1.00.5 (30 minutes)
2.510
  • Stand-up time decreases sharply with increasing unsupported span.
  • Applies primarily to saturated rock masses in slopes.

Influencing Parameters:

  • Rock Mass Cohesion (kg/cm²)
  • Internal Friction Angle (°)
  • Rock Mass Quality (Q) [IS 13365 Part 2]
  • Unit Weight (Y) in g/cc
  • Joint Roughness (Jr) & Joint Alteration (Ja) Numbers

Conceptual Relationship (Fig.1):

graph LR
  A[Unsupported Span] --> B[Stand-up Time]
  C[Rock Mass Quality] --> B
  D[Arch Shape] --> B
  E[Controlled Blasting] --> B
  B --> F[Safe Excavation Time]

Practical Use:

  • Determine effective span.
  • Use Fig.1 or Table above for initial stand-up time.
  • Adjust based on rock parameters and excavation method.
  • Use stand-up time for planning support installation to avoid collapse.

Summary:
Stand-up time is crucial for tunnel safety, varying inversely with unsupported span and directly with rock quality and support methods. Use IS 13365 Part 1 guidelines combined with rock mass parameters for design.

9Adjustment for Joint Orientation

Adjustment for Joint Orientation (IS 13365 Part 1)

Key Points from Clause 3.1.6 & Annex B, C:

  • Orientation of discontinuities is defined by strike (angle from magnetic north) and dip (angle between horizontal and discontinuity plane).
  • Record strike and dip for critical joint sets unfavorable to the structure.
  • Compare joint orientation with tunnel axis, slope face, or foundation alignment.
  • Use Annex C, Tables C1 & C2 to assess joint favourability for tunnels and dam foundations.
  • Adjust the basic Rock Mass Rating (RMR) by applying orientation factors from Item VII, Annex B.

Procedure for Adjustment:

  1. Determine joint strike and dip relative to tunnel axis.
  2. Classify joint favourability using Tables C1 (tunnels) or C2 (foundations).
  3. Apply orientation adjustment factor to the basic RMR:

[ RMR_{adjusted} = RMR_{basic} \times F_{orientation} ]

Where ( F_{orientation} ) is from Annex B (Item VII).


Typical Orientation Adjustment Factors (Example):

Joint OrientationFavorabilityFactor (F_{orientation})
FavorableGood1.0
ModerateAverage0.85
UnfavorablePoor0.7

Summary Diagram:

flowchart TD
    A[Record Joint Strike & Dip] --> B[Compare with Tunnel Axis]
    B --> C{Use Tables C1/C2}
    C -->|Favorable| D[Factor = 1.0]
    C -->|Moderate| E[Factor = 0.85]
    C -->|Unfavorable| F[Factor = 0.7]
    D --> G[Calculate Adjusted RMR]
    E --> G
    F --> G

References:

  • Annex B (Item VI & VII): Strike, dip recording & orientation adjustment.
  • Annex C (Tables C1 & C2): Joint favourability classification.
  • Clause 4.5: Separate RMR for different tunnel orientations.

This adjustment ensures RMR reflects realistic stability conditions based on

Annex AList of Referred Indian Standards

IS 13365 Part 1 (1998) — List of Referred Indian Standards

This standard references several IS codes related to rock mass characterization and design:

IS No.Title
IS 8764 : 1978Method of determination of point load strength index of rocks
IS 8764 (Part 2) : 1987Spacing
IS 8764 (Part 3) : 1987Persistence
IS 9143 : 1979Method for determination of unconfined compressive strength of rock materials
IS 9143 (Part 8) : 1987Seepage
IS 9143 (Part 11) : 1987Core recovery and rock quality
IS 9221 : 1979Method for determination of modulus of elasticity and Poisson's ratio of rock materials in uniaxial compression
IS 12070 : 1987Code of practice for design and construction of shallow foundation on rock
IS 13365 (Part 2) : 1992Quantitative classification systems of rock mass—Guidelines: Rock mass quality for prediction of support pressure in underground openings
IS 11315 (Part 1) : 1987Method for quantitative description of discontinuities in rock mass: Orientation

Key Notes:

  • These referenced standards provide methods for testing rock strength, elasticity, discontinuities, and classification.
  • IS 13365 Part 1 uses these for rock mass classification and design guidance.
  • Always check for the latest editions of these standards.

Example: Rock Mass Number (N) Calculation (from IS 13365 Part 1)

[ N = Q \times SRF ]

Where:

  • Q = Rock Quality Designation (from rock mass classification)
  • SRF = Stress Reduction Factor (accounts for rock stress and excavation conditions)

flowchart LR
    A[Rock Mass Parameters] --> B[Point Load Strength Index (IS 8764)]
    A --> C[Unconfined Compressive Strength (IS 9143)]
    A --> D[Modulus of Elasticity & Poisson's Ratio (IS 9221)]
    B --> E[Rock Quality Designation (Q)]
    C --> E
Annex BData Sheet for Geomechanical Classification of Rock Masses

IS 13365 Part 1: Data Sheet & Key Formulas for Geomechanical Classification of Rock Masses


1. Rock Mass Rating (RMR) & Engineering Properties (Clause 5.1)

  • Rock mass rating (RMR) correlates with engineering properties (strength, deformability).
  • Use Table 1 (Clause 5.1) for ranges of properties based on RMR.
  • Interpret properties within recommended ranges for given RMR.

2. Prediction of Tunnelling Conditions (Clause 23.4)

ConditionFormula for H (Overburden in m)
Low squeezing( H < 23.4 \times N^{0.89} \times B^{-0.1} \times 1000 \times B^{-0.1} )
Moderate squeezing( 275 \times N^{0.33} \times B^{-0.1} < H < 450 \times N^{0.33} \times B^{-0.1} )
High squeezing( 450 \times N^{0.33} \times B^{-0.1} < H < 630 \times N^{0.33} \times B^{-0.1} )
Very high squeezing( H > 630 \times A^{0.33} \times B^{-0.1} )
  • N = rock mass number (Clause 4.3), B = tunnel width (m), H = overburden (m).

3. In-situ Modulus of Deformability, ( E ) (GPa)

Three empirical formulas:

[ \begin{aligned} E &= 2 \times RMR - 100 \ E &= 10 \times \frac{RMR - 10}{40} \ E &= 10 \text{ to } 40 \times \log_{10} Q \end{aligned} ]

  • (RMR): Rock Mass Rating
  • (Q): Rock mass quality number

4. Recommended Mohr Envelopes for Jointed Rock Masses (Table 2, Clause 5.1.6)

  • Rock mass quality classified by RMR and Q values:
Annex CAssessment of Joint Favorability for Tunnels and Foundations

IS 13365 Part 1: Assessment of Joint Favorability for Tunnels and Foundations

Key Formulas & Correlations for Tunneling Conditions (Clause 5.1.8)

Ground ConditionCorrelation (H = overburden, N = rock mass number, B = tunnel width)
Self-supporting( H < 23.4 \times N^{0.89} \times B^{-0.1} ) and ( H < 1000 \times B^{-0.1} )
Non-squeezing( 23.4 \times N^{0.88} \times B^{-0.1} < H < 275 \times N^{0.33} \times B^{-0.1} )
Mild squeezing( 275 \times N^{0.33} \times B^{-0.1} < H < 450 \times N^{0.33} \times B^{-0.1} )
Moderate squeezing( 450 \times N^{0.33} \times B^{-0.1} < H < 630 \times N^{0.33} \times B^{-0.1} )
High squeezing( H > 630 \times N^{0.33} \times B^{-0.1} )

Shear Strength of Jointed Rock Masses (Clause 5.1.6)

[ \tau = A(\sigma_n + T)^B, \quad \text{with } \tau=0 \text{ if } \sigma_n < 0 ]

  • (\tau) = shear strength
  • (\sigma_n) = normal stress on joint
  • (A, T, B) = constants from Table 2 (vary with rock quality & saturation)
  • (q_c) = uniaxial compressive strength of intact rock

In-situ Modulus of Deformability (E) (GPa)

  • (E = 2 \times RMR - 100)
  • (E = 10 \times \frac{RMR - 10}{40})
  • (E = 10 \text{ to } 40 \times \log
Annex DCommittee Composition

IS 13365 Part 1: Committee Composition - Key Details

The Rock Mechanics Sectional Committee, CED 48 is responsible for formulating IS 13365 Part 1. The committee comprises experts from academia, government departments, research institutes, and industry.

Committee Structure (Annex D Summary):

RoleRepresentative Organization/Person
ChairmanProf. Bhawani Singh, University of Roorkee
Members include:- Irrigation Departments (UP, Haryana, Punjab, Maharashtra, Gujarat)
- Central Mining Research Institute (CSIR)
- Central Building Research Institute (CSIR)
- Geological Survey of India
- Central Water and Power Research Station
- Hindustan Construction Co Ltd
- National Thermal Power Corporation
- Indian Institute of Technology, New Delhi
- Central Ground Water Board
- Indian Geotechnical Society
- BIS Director General (Ex-officio Member)
Member SecretaryDirector (Civil Engg), BIS

Notes:

  • The committee includes technical experts and government officials ensuring a comprehensive approach.
  • The committee composition is detailed in Annex D of IS 13365 Part 1.
  • This committee oversees rock mechanics standards including classification and rating systems.

If you need formulas or tables related to rock mass classification (RMR, RQD, discontinuity spacing), please specify!

Popular Questions About IS 13365 Part 1

?What parameters are used to calculate the Rock Mass Rating (RMR)?

The Rock Mass Rating (RMR) in IS 13365 Part 1 is calculated using these key parameters:

  1. Uniaxial Compressive Strength (UCS) of Intact Rock
  2. Rock Quality Designation (RQD)
  3. Spacing of Discontinuities
  4. Condition of Discontinuities
  5. Groundwater Conditions

These five parameters are summed to get the Basic Rock Mass Rating (RMR_basic) (Clause 3.1.1).

Then, adjustments are made for:

  1. Orientation of Discontinuities (Clause 4.1, Annex B)

The Rock Condition Rating (RCR) is the sum of parameters 2 to 5, excluding UCS and orientation effects, representing the modified RMR.


Summary Table for RMR Parameters

ParameterDescription
I. UCSStrength of intact rock
II. RQD% of core recovery > 10 cm length
III. Spacing of DiscontinuitiesAverage distance between joints
IV. Condition of DiscontinuitiesRoughness, weathering, etc.
V. Groundwater ConditionsDry, damp, flowing, etc.
VI. Orientation AdjustmentJoint orientation relative to excavation

Loading diagram...

This RMR helps estimate support requirements, stand-up time, and excavation methods.

?How does groundwater condition affect the RMR and rock mass properties?

Effect of Groundwater on RMR and Rock Mass Properties (IS 13365 Part 1)

  • RMR Determination: Groundwater or pore water pressure should not be double-counted. If pore water pressure is considered in structural analysis, it should be excluded from RMR adjustments (Clause 4.1).

  • Rating Adjustment: Saturation generally reduces rock mass strength and modulus, especially in poor rock masses with water-sensitive minerals (Clause 5.1.3.2). Saturated poor rocks show significant reduction in deformability over time.

  • Modulus of Deformation (Ed): For saturated soft rock masses, Ed decreases due to water presence and depends on depth and RMR:

    [ E_d = 0.3z \times 10^{(RMR-20)/38} \quad \text{(GPa)}, \quad z = \text{depth (m)} ]

  • Mohr Envelope Parameters: Table 5.1.6 shows strength parameters decrease with saturation (S=1), e.g., cohesion and friction angle reduce in saturated conditions.

  • Practical Recommendation: Conduct uniaxial jacking tests soon after excavation in saturated zones to capture reduced stiffness (Clause 5.1.3.2).


Summary Table: Groundwater Impact on Rock Mass

PropertyDry Rock MassSaturated Rock MassEffect of Saturation
RMRBase ratingAdjusted carefully, avoid double countingMay decrease strength rating
Modulus of DeformationHigher (Ed from RMR)Reduced, especially in poor rocksSignificant reduction
Strength ParametersHigher cohesion/frictionLower cohesion/friction (see Table 5.1.6)Decrease in shear strength

Loading diagram...

Key Takeaway: Groundwater saturation lowers rock mass strength and deformability,

?What is the recommended procedure for assessing discontinuities in rock masses?

Assessment Procedure for Discontinuities in Rock Masses (IS 13365 Part 1)

  1. Identify and Measure Discontinuities (Clause 3.1.3)

    • Measure linear spacing between adjacent discontinuities (joints, faults, foliations, etc.).
    • Record spacing for all sets.
    • Use Annex B (Item III) for rating spacing.
  2. Evaluate Condition of Discontinuities (Clause 3.1.4)

    • Assess surface roughness, separation, length/continuity.
    • Note weathering of wall rock and infilling material.
    • Refer to Annex B (Item IV) for condition rating.
    • Use IS 11315 (Part 4 & 5) for terminology.
  3. Determine Orientation (Clause 3.1.6)

    • Record strike (relative to magnetic north) and dip angle.
    • Compare orientation with tunnel axis, slope face, or foundation alignment.
    • Use Annex B (Item VI) for recording format.
    • Assess favorability using Annex C Tables C1 (tunnels) and C2 (dams).
    • Adjust rock mass rating (RMR) based on orientation (Annex B, Item VII).

Summary Table for Discontinuity Assessment

ParameterMeasurement/AssessmentReference for Rating
SpacingLinear distance between jointsAnnex B (Item III)
ConditionRoughness, weathering, infillingAnnex B (Item IV), IS 11315
OrientationStrike & dip anglesAnnex B (Item VI), Annex C

Loading diagram...

This systematic approach ensures a comprehensive evaluation of discontinuities for rock mass classification and design.

?How can RMR be used to estimate the modulus of deformation of rock masses?

Estimating Modulus of Deformation (Ed) from RMR (IS 13365 Part 1)

  1. Modulus Reduction Factor (MRF) Method (Clause 5.1.3.1):
    [ E_d = E \times MRF ]

    • (E) = Modulus of elasticity of intact rock (from IS 9221)
    • (MRF) = Modulus reduction factor from Fig. 2, based on RMR
    • Applicable for hard jointed rock
  2. Direct Correlations (Clause 5.1.3.2):

    • For hard rock masses ((q_c \geq 50 \text{ MPa})):
      [ E_d = 2 \times RMR - 100 \quad \text{(GPa)} ] or
      [ E_d = \frac{10(RMR - 10)}{40} \quad \text{(GPa)} ]

    • For dry soft rock masses ((q_c < 50 \text{ MPa})) at depth (z \geq 50m):
      [ E_d = 0.3 \times z^{a} \times 10^{\frac{RMR - 20}{38}} \quad \text{(GPa)}, \quad a = 0.16 \text{ to } 0.30 ]

  3. Notes:

    • For poor, water-sensitive rocks, modulus decreases after saturation/time.
    • Use undamaged rock face for RMR estimation (Clause 4.6).
    • For dam foundations, perform uniaxial jacking tests for accurate (E_d).

Summary Table:

Rock TypeFormula for (E_d) (GPa)Notes
Hard rock ((q_c \geq 50))(2 \times RMR - 100) or (\frac{10(RMR-10)}{40})Simple direct correlation
Dry soft rock ((q_c < 50))(0.3 z^{a} 10^{\frac{RMR-
?What empirical correlations does the standard provide for predicting support pressure in tunnels?

IS 13365 Part 1 provides empirical correlations for estimating short-term support pressure in tunnels, especially for arched openings using steel rib supports in conventional blasting:

Key Empirical Correlation (Clause 7.5)

[ \text{Proof} = \frac{7.5 \times B^{0.1} \times H^{0.5} - \text{RMR}}{2 \times \text{RMR}} \quad \text{(kg/cm}^2) ]

  • B = Span of tunnel opening (m)
  • H = Overburden depth (m, typically > 50 m)
  • RMR = Rock Mass Rating

This formula estimates the short-term roof support pressure (Proof) considering rock mass quality.

Ground Condition Prediction (Clause 5.1.8)

Tunnelling conditions relate to depth (H) and span (B) via:

ConditionCorrelation Range (H, B)
Self-supporting(H < 23.4 \times B^{-0.1})
Non-squeezing(23.4 \times B^{-0.1} < H < 275 \times B^{-0.1})
Mild squeezing(275 \times B^{-0.1} < H < 450 \times B^{-0.1})
Moderate squeezing(450 \times B^{-0.1} < H < 630 \times B^{-0.1})
High squeezing(H > 630 \times B^{-0.1})

Notes:

  • The Q-system (IS 13365 Part 2) with correct Stress Reduction Factor (SRF) refines support pressure predictions.
  • Rock mass parameters like unit weight (Y), joint roughness (J_r), and joint alteration (J_a) influence RMR and thus support pressure.

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