IS 11315 Part 3 (1987) provides a standardized method for quantitatively describing the persistence of discontinuities in rock masses. It guides engineers in assessing the trace length and continuity of rock discontinuities, which are critical for evaluating rock stability in slopes, tunnels, and foundations. This standard is essential for geotechnical engineers, rock mechanics specialists, and civil engineers involved in rock mass characterization and stability analysis.
Overview
IS 11315 Part 3 (1987) provides a standardized method for quantitatively describing the persistence of discontinuities in rock masses. It guides engineers in assessing the trace length and continuity of rock discontinuities, which are critical for evaluating rock stability in slopes, tunnels, and foundations. This standard is essential for geotechnical engineers, rock mechanics specialists, and civil engineers involved in rock mass characterization and stability analysis.
Audience
Contents
Structure
IS 11315 Part 3 - Introduction: Key Formulas, Tables & Specs
| Persistence Level | Length (m) |
|---|---|
| Very Low | < 1 |
| Low | 1 – 3 |
| Medium | 3 – 10 |
| High | 10 – 20 |
| Very High | > 20 |
Using Mohr envelope (linear shear strength):
[ C = \frac{( \sigma_c - \sigma_t )}{6} ]
Where:
Interpretation: Cohesion ≈ 1/6 of UCS.
| Quantity | Unit | Symbol |
|---|---|---|
| Length | metre | m |
| Mass | kilogram | kg |
| Time | second | s |
| Force | newton | N |
| Pressure, stress | pascal | Pa |
| Energy | joule | J |
flowchart TD
A[Discontinuity Persistence] --> B{Persistence Level}
B -->|<1 m| C[Very Low]
B -->|1-3 m| D[Low]
B -->
IS 11315 Part 3 — Scope: Key Specifications & Tables
| Persistence Level | Length (m) |
|---|---|
| Very Low Persistence | < 1 |
| Low Persistence | 1 – 3 |
| Medium Persistence | 3 – 10 |
| High Persistence | 10 – 20 |
| Very High Persistence | > 20 |
graph LR
A[Very Low <1m] --> B[Low 1-3m]
B --> C[Medium 3-10m]
C --> D[High 10-20m]
D --> E[Very High >20m]
Use this scope to estimate and classify rock discontinuity persistence consistently.
IS 11315 Part 3 — Key Definitions & Specifications
Persistence refers to the length of potential failure surfaces in rock masses, categorized as:
| Persistence Level | Length (m) |
|---|---|
| Very Low | < 1 |
| Low | 1 – 3 |
| Medium | 3 – 10 |
| High | 10 – 20 |
| Very High | > 20 |
| Quantity | Unit | Symbol | Definition |
|---|---|---|---|
| Length | metre | m | |
| Mass | kilogram | kg | |
| Time | second | s | |
| Force | newton | N | 1 N = 1 kg·m/s² |
| Pressure, Stress | pascal | Pa | 1 Pa = 1 N/m² |
| Energy | joule | J | 1 J = 1 N·m |
| Power | watt | W | 1 W = 1 J/s |
flowchart LR
A[Discontinuity Persistence] --> B{Length (m)}
B -->|<1| VeryLow[Very Low Persistence]
B -->|1-3| Low[Low Persistence]
B -->|3-10| Medium[Medium Persistence]
B -->|10-20| High[High Persistence]
B -->|>20| VeryHigh[Very High Persistence]
This concise summary covers key definitions, units, and persistence classification per IS 11315 Part 3.
1. Persistence of Failure Surfaces (Clause 5.4):
2. Persistence Classification (Clause 4.3):
| Persistence Level | Length (m) |
|---|---|
| Very Low Persistence | < 1 m |
| Low Persistence | 1 – 3 m |
| Medium Persistence | 3 – 10 m |
| High Persistence | 10 – 20 m |
| Very High Persistence | > 20 m |
3. SI Units and Definitions:
| Quantity | Unit | Symbol | Definition |
|---|---|---|---|
| Length | metre | m | |
| Force | newton | N | 1 N = 1 kg·m/s² |
| Pressure, Stress | pascal | Pa | 1 Pa = 1 N/m² |
| Energy | joule | J | 1 J = 1 N·m |
| Power | watt | W | 1 W = 1 J/s |
| Frequency | hertz | Hz | 1 Hz = 1 s⁻¹ |
4. Rounding Off (Clause 0.6):
flowchart TD
A[Estimate Persistence] --> B{Round Up?}
B -- Yes --> C[Round to next 10%]
B -- No --> D[Use exact value]
C --> E[Classify Persistence]
D --> E
E --> F{Persistence Level}
F -->|<1 m| G[Very Low Persistence]
F -->|1-3 m| H[Low Persistence]
F -->|3-10 m| I[Medium Persistence]
F -->|10-20 m| J[High Persistence]
F -->|>20 m| K[Very High Persistence]
Summary:
IS 11315 Part 3: Procedure Key Points
| Persistence Level | Persistence Length |
|---|---|
| Very Low Persistence | < 1 m |
| Low Persistence | 1 - 3 m |
| Medium Persistence | 3 - 10 m |
| High Persistence | 10 - 20 m |
| Very High Persistence | > 20 m |
graph LR
A[Very Low Persistence] -->|<1 m| B[Low Persistence]
B -->|1-3 m| C[Medium Persistence]
C -->|3-10 m| D[High Persistence]
D -->|10-20 m| E[Very High Persistence]
E -->|>20 m| F[Failure Surface]
This classification helps in assessing the continuity and potential impact of discontinuities in rock or soil mass during stability analysis.
IS 11315 Part 3 — Presentation of Results: Key Points
| Persistence Level | Length (m) |
|---|---|
| Very low persistence | < 1 m |
| Low persistence | 1 – 3 m |
| Medium persistence | 3 – 10 m |
| High persistence | 10 – 20 m |
| Very high persistence | > 20 m |
Cohesion, C, estimated from Mohr envelope assuming linear shear strength:
[ C = \frac{F_c - \sigma_t}{6} ]
where:
This implies cohesion ≈ 1/6 of unconfined compressive strength.
flowchart LR
A[Discontinuity Persistence Estimation] --> B{Persistence Level?}
B -->|<1 m| C[Very Low Persistence]
B -->|1-3 m| D[Low Persistence]
B -->|3-10 m| E[Medium Persistence]
B -->|10-20 m| F[High Persistence]
B -->|>20 m| G[Very High Persistence]
A --> H[Round Persistence to nearest 10%]
H --> I[Assume 100% if uncertain]
I --> J[Calculate
Key Notes & Recommendations from IS 11315 Part 3 (1987):
Persistence Estimation (Clause 5.4):
Discontinuity Data (Clause 4.5):
Persistence & Shear Strength:
[ C = \frac{F_c - \sigma_t}{6} ]
where:
(F_c) = uniaxial compressive strength,
(\sigma_t) = tensile strength (assumed (F_c / \sigma_t = 9)).
Units:
| Parameter | Symbol | Typical Value/Formula |
|---|---|---|
| Uniaxial compressive strength | (F_c) | Given by rock test |
| Tensile strength | (\sigma_t) | (F_c / 9) (assumed) |
| Cohesion from intact bridges | (C) | (C = \frac{F_c - \sigma_t}{6}) |
| Persistence rounding | — | Round up to nearest 10% (e.g., 92% → 100%) |
flowchart LR
A[Discontinuity Data] --> B[Record termination data (x, r or d)]
B --> C[Estimate persistence]
C --> D{Is persistence < 100%?}
D -- Yes --> E[Consider stepped failure surfaces]
D -- No --> F[Assume full persistence]
E --> G[Estimate shear strength using Mohr envelope]
F --> G
G --> H[Calculate cohesion
Frequently Asked
According to IS 11315 Part 3 (1987), persistence of rock discontinuities is quantitatively measured by:
[ C = \frac{F_c}{6} ]
Where:
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Summary: Persistence = measured trace length between terminations, statistically analyzed, and conservatively interpreted for design safety.
Based on IS 11315 Part 3, discontinuity sets are classified by persistence (trace length observed on rock exposure) as follows:
| Classification | Description | Typical Trace Length (measured with ≥10 m tape) |
|---|---|---|
| Persistent | Long, continuous discontinuities extending over large areas or penetration lengths | Typically > 10 m |
| Sub-persistent | Moderate length discontinuities, less continuous | Several meters, but less than persistent |
| Non-persistent | Short, discontinuities terminating quickly in rock or against others | Usually < 1 m |
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This classification helps in rock mass characterization and engineering design.
Effect of Persistence on Stability Assessment (IS 11315 Part 3)
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Summary: Persistence is a key parameter controlling failure surface development and must be carefully assessed for reliable stability analysis.
IS 11315 Part 3 - Measuring Discontinuity Persistence
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This approach ensures reliable persistence data for rock mass evaluation per IS 11315 Part 3.
Presentation and Interpretation of Persistence Data (IS 11315 Part 3)
Persistence Definition: Persistence is the observed trace length of discontinuities, indicating their areal extent or penetration length in rock exposures (Clauses 0.5, 3.6).
Data Recording: Record termination data (x, r or d) for each end of discontinuities along with their length in meters (Clause 4.5).
Estimation: Persistence of potential failure surfaces, including stepped surfaces, should be estimated and rounded upwards to the nearest 10% (e.g., 92% → 100%) for conservatism (Clause 5.4).
Interpretation Notes:
Shear Strength Estimation: Cohesion from intact rock bridges can be approximated as:
[ C = \frac{F_c}{6} ]
where (F_c) = uniaxial compressive strength (assuming ( \sigma_c / \sigma_t = 9 )).
| Parameter | Unit | Notes |
|---|---|---|
| Discontinuity length | meters | Measured with tape ≥10 m |
| Termination data (x, r, d) | meters | Recorded for each discontinuity end |
| Persistence estimate | % | Rounded up to nearest 10%, conservatively |
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This approach ensures conservative, reliable interpretation of persistence data in rock engineering reports per IS 11315 Part 3.
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