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.
Overview
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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Contents
Structure
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):
Rock Mass Behavior Classification (Fig. 4):
Based on ( N ), tunnel depth, and width, ground conditions are categorized as:
Referenced IS Codes (Annex A):
| IS No. | Title |
|---|---|
| 8764:1978 | Point Load Strength Index of Rocks |
| 9143:1979 | Unconfined Compressive Strength of Rock Materials |
| 9221:1979 | Modulus of Elasticity and Poisson's Ratio of Rock |
| 11315 (Parts 1-3) | Quantitative Description of Discontinuities |
| Rock Mass Number (N) | Ground Condition |
|---|---|
| High | Self-supporting |
| Moderate | Non-squeezing |
| Low | Mild 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
IS 13365 Part 1 (1998) - Key References, Formulas & Tables
Rock Mass Number:
[
N = Q \times SRF
]
where Q = Rock Quality, SRF = Stress Reduction Factor.
Tunneling Conditions (Clause 5.1.8 / Fig.4):
| Ground Condition | Correlation (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} ) |
[ E = 2 \times RMR - 100 ] [ E = 10 \times \frac{(RMR - 10)}{40} ] [ E = 10 \text{ to } 40 \times \log_{10} Q ]
| IS No. | Title |
|---|---|
| IS 8764:1978 | Point Load Strength Index of Rocks |
IS 13365 Part 1: Collection of Field Data (Clause 3.1 & 3.1.1)
Key Parameter:
Testing Standards:
Data Recording:
Rating System (Annex B, Item I):
| UCS (MPa) | Rock Strength Rating |
|---|---|
| > 250 | Very High |
| 100 – 250 | High |
| 50 – 100 | Medium |
| < 50 | Low |
Important Note:
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.
Three empirical correlations (E in GPa):
| Formula No. | Formula | Reference |
|---|---|---|
| (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 |
| Condition | Range 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.
| RMR Range | Rock Quality (Q) | Description | |-----------
Engineering Properties of Rock Masses (IS 13365 Part 1)
| RMR Range | Class | Rock Mass Quality | Avg. Stand-up Time | Cohesion (kg/cm²) | Friction Angle (°) |
|---|---|---|---|---|---|
| 100-81 | I | Very Good | 10 years (15 m span) | >4 | >45 |
| 80-61 | II | Good | 6 months (8 m span) | 3-4 | 35-45 |
| 60-41 | III | Fair | 1 week (5 m span) | 2-3 | 25-35 |
| 40-21 | IV | Poor | 10 hours (2.5 m span) | 1-2 | 15-25 |
| <20 | V | Very Poor | 30 minutes (1 m span) | <1 | 15 |
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:
[ q_{c, \text{mass}} = 70 \text{ MPa (approx.) for } Q \leq 10, J_w = 1
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 Condition | Correlation 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} ) |
[ \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} ]
[ \sigma_v = 0.27 \times H \quad (\text{kg/cm}^2) ]
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) ]
| Ground Condition | Correlation 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}) |
flowchart TD
A[Input: Span
Stand-up Time for Unsupported Span
(IS 13365 Part 1:1998)
| Unsupported Span (m) | Stand-up Time (hours) |
|---|---|
| 1.0 | 0.5 (30 minutes) |
| 2.5 | 10 |
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]
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.
Key Points from Clause 3.1.6 & Annex B, C:
[ RMR_{adjusted} = RMR_{basic} \times F_{orientation} ]
Where ( F_{orientation} ) is from Annex B (Item VII).
| Joint Orientation | Favorability | Factor (F_{orientation}) |
|---|---|---|
| Favorable | Good | 1.0 |
| Moderate | Average | 0.85 |
| Unfavorable | Poor | 0.7 |
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
This adjustment ensures RMR reflects realistic stability conditions based on
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 : 1978 | Method of determination of point load strength index of rocks |
| IS 8764 (Part 2) : 1987 | Spacing |
| IS 8764 (Part 3) : 1987 | Persistence |
| IS 9143 : 1979 | Method for determination of unconfined compressive strength of rock materials |
| IS 9143 (Part 8) : 1987 | Seepage |
| IS 9143 (Part 11) : 1987 | Core recovery and rock quality |
| IS 9221 : 1979 | Method for determination of modulus of elasticity and Poisson's ratio of rock materials in uniaxial compression |
| IS 12070 : 1987 | Code of practice for design and construction of shallow foundation on rock |
| IS 13365 (Part 2) : 1992 | Quantitative classification systems of rock mass—Guidelines: Rock mass quality for prediction of support pressure in underground openings |
| IS 11315 (Part 1) : 1987 | Method for quantitative description of discontinuities in rock mass: Orientation |
[ N = Q \times SRF ]
Where:
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
IS 13365 Part 1: Data Sheet & Key Formulas for Geomechanical Classification of Rock Masses
| Condition | Formula 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} ) |
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} ]
IS 13365 Part 1: Assessment of Joint Favorability for Tunnels and Foundations
| Ground Condition | Correlation (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} ) |
[ \tau = A(\sigma_n + T)^B, \quad \text{with } \tau=0 \text{ if } \sigma_n < 0 ]
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.
| Role | Representative Organization/Person |
|---|---|
| Chairman | Prof. 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 Secretary | Director (Civil Engg), BIS |
If you need formulas or tables related to rock mass classification (RMR, RQD, discontinuity spacing), please specify!
Frequently Asked
The Rock Mass Rating (RMR) in IS 13365 Part 1 is calculated using these key parameters:
These five parameters are summed to get the Basic Rock Mass Rating (RMR_basic) (Clause 3.1.1).
Then, adjustments are made for:
The Rock Condition Rating (RCR) is the sum of parameters 2 to 5, excluding UCS and orientation effects, representing the modified RMR.
| Parameter | Description |
|---|---|
| I. UCS | Strength of intact rock |
| II. RQD | % of core recovery > 10 cm length |
| III. Spacing of Discontinuities | Average distance between joints |
| IV. Condition of Discontinuities | Roughness, weathering, etc. |
| V. Groundwater Conditions | Dry, damp, flowing, etc. |
| VI. Orientation Adjustment | Joint orientation relative to excavation |
Loading diagram...
This RMR helps estimate support requirements, stand-up time, and excavation methods.
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).
| Property | Dry Rock Mass | Saturated Rock Mass | Effect of Saturation |
|---|---|---|---|
| RMR | Base rating | Adjusted carefully, avoid double counting | May decrease strength rating |
| Modulus of Deformation | Higher (Ed from RMR) | Reduced, especially in poor rocks | Significant reduction |
| Strength Parameters | Higher cohesion/friction | Lower cohesion/friction (see Table 5.1.6) | Decrease in shear strength |
Loading diagram...
Key Takeaway: Groundwater saturation lowers rock mass strength and deformability,
Assessment Procedure for Discontinuities in Rock Masses (IS 13365 Part 1)
Identify and Measure Discontinuities (Clause 3.1.3)
Evaluate Condition of Discontinuities (Clause 3.1.4)
Determine Orientation (Clause 3.1.6)
| Parameter | Measurement/Assessment | Reference for Rating |
|---|---|---|
| Spacing | Linear distance between joints | Annex B (Item III) |
| Condition | Roughness, weathering, infilling | Annex B (Item IV), IS 11315 |
| Orientation | Strike & dip angles | Annex B (Item VI), Annex C |
Loading diagram...
This systematic approach ensures a comprehensive evaluation of discontinuities for rock mass classification and design.
Estimating Modulus of Deformation (Ed) from RMR (IS 13365 Part 1)
Modulus Reduction Factor (MRF) Method (Clause 5.1.3.1):
[
E_d = E \times MRF
]
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
]
Notes:
| Rock Type | Formula 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- |
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:
[ \text{Proof} = \frac{7.5 \times B^{0.1} \times H^{0.5} - \text{RMR}}{2 \times \text{RMR}} \quad \text{(kg/cm}^2) ]
This formula estimates the short-term roof support pressure (Proof) considering rock mass quality.
Tunnelling conditions relate to depth (H) and span (B) via:
| Condition | Correlation 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}) |
Loading diagram...
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