IS 11315 Part 5 (1987) specifies the method for quantitatively evaluating the compressive strength of rock mass discontinuity walls. It guides engineers in assessing wall strength using field tests like the Schmidt hammer and manual index tests, considering factors such as weathering and rock density. This standard is essential for geotechnical engineers, rock mechanics specialists, and civil engineers involved in rock mass characterization for construction, mining, and infrastructure projects.
Overview
IS 11315 Part 5 (1987) specifies the method for quantitatively evaluating the compressive strength of rock mass discontinuity walls. It guides engineers in assessing wall strength using field tests like the Schmidt hammer and manual index tests, considering factors such as weathering and rock density. This standard is essential for geotechnical engineers, rock mechanics specialists, and civil engineers involved in rock mass characterization for construction, mining, and infrastructure projects.
Audience
Contents
Structure
IS 11315 Part 5 - Scope: Key Formulas, Tables & Specifications
Defines classification and assessment of rock mass weathering, rock material weathering, and rock strength for engineering purposes.
| Term | Description | Grade |
|---|---|---|
| Fresh | No visible weathering, slight discoloration on discontinuities | I |
| Moderately weathered | <50% decomposed/disintegrated, fresh/discoloured rock as continuous/core | III |
| Highly weathered | >50% decomposed/disintegrated, discontinuous framework/core stones | IV |
| Completely weathered | All decomposed/disintegrated, original mass structure intact | V |
| Residual soil | All converted to soil, fabric destroyed, volume change, not transported | VI |
| Term | Description |
|---|---|
| Fresh | No visible sign of weathering |
| Discoloured | Colour changed; specify degree and affected minerals |
| Decomposed | Weathered to soil; fabric intact, mineral grains decomposed |
| Disintegrated | Weathered to soil; fabric intact, friable, grains not decomposed |
| Grade | Description | Field ID | Uniaxial Compressive Strength (MPa) |
|---|---|---|---|
| S1-S6 | Clay types (soft to hard) | Penetration varies from fist to thumb-nail | <0.025 to >0.50 |
| R0-R6 | Rock strength (extremely weak to extremely strong) | Indentation/fracture by hammer or knife | 0.25 to >250 |
| Term | Description | Grade |
|---|---|---|
| Fresh | No visible weathering; slight discoloration on major discontinuities | I |
| Moderately weathered | <50% rock decomposed/disintegrated; fresh/discoloured rock as continuous framework/core stones | III |
| Highly weathered | >50% rock decomposed/disintegrated; discontinuous framework/core stones | IV |
| Completely weathered | All rock decomposed/disintegrated; original structure largely intact | V |
| Residual soil | All rock converted to soil; structure & fabric destroyed; volume change, soil not transported | VI |
| Term | Description |
|---|---|
| Fresh | No visible weathering |
| Discoloured | Colour changed; specify degree and mineral affected |
| Decomposed | Weathered to soil; original fabric intact but mineral grains decomposed |
| Disintegrated | Weathered to soil; fabric intact; rock friable but mineral grains not decomposed |
| Grade | Description | Field ID | Approx. UCS (MPa) |
|---|---|---|---|
| S1 | Very soft clay | Penetrated by fist | <0.025 |
| S2 | Soft clay | Penetrated by thumb | 0.025–0.05 |
| S3 | Firm clay | Penetrated by thumb with moderate effort | 0.05–0.10 |
| S4 | Stiff clay | Indented by thumb, penetrated with effort | 0.10–0.25 |
| S5 | Very stiff clay | Indented by thumb-nail | 0.25–0.50 |
| S6 | Hard clay | Indented with difficulty by thumb-nail | >0.50 |
| R0 | Extremely weak rock | Indented by thumb-nail |
IS 11315 Part 5 – Factors Affecting Wall Strength
| Table 1 | Strength variation with weathering of rock mass |
|---|---|
| Fresh | Highest strength |
| Slightly weathered | Moderate strength |
| Highly weathered | Low strength |
| Table 2 | Strength variation with rock material type |
|---|---|
| Igneous | High strength |
| Sedimentary | Moderate strength |
| Metamorphic | Variable strength depending on alteration |
| Table 3 | Manual Index Tests for Rock Strength Estimation |
|---|---|
| Point Load Test | Provides uniaxial strength index |
| Unconfined Compressive Strength (UCS) | Direct strength measure |
[ \sigma_c = k \times R ]
flowchart LR
A[Rock Mass Weathering] --> B[Strength Reduction]
C[Rock Material Type] --> B
D[Manual Index Tests] --> E[Strength Estimation]
F[Schmidt Hammer Test] --> E
B --> E
Summary: Wall strength depends on rock weathering, rock type, and test-based strength indices (manual and Schmidt hammer). Use Tables 1-3 and Fig.1 for assessment.
IS 11315 Part 5 (1987) - Equipment and Test Methods Key Points
[ \text{UCS} = f(\text{Corrected Rebound Number}) ]
| Rebound Number (Raw) | Corrected Rebound Number | Estimated UCS (MPa) |
|---|---|---|
| 30 | 28 | 50 |
| 40 | 38 | 90 |
| 50 | 48 | 140 |
flowchart LR
A[Geological Hammer] --> B[Rock Surface Preparation]
C[Schmidt Hammer] --> D[Rebound Number Measurement]
D --> E[Correction using Table]
E --> F[Estimate UCS using Graph]
G[Sample] --> H[Dry Density Measurement]
H --> I[Oven, Balance, Pyknometer]
This ensures standardized, reproducible rock strength evaluation and reporting per IS 11315 Part 5.
IS 11315 Part 5 - Test Procedures and Data Collection: Key Formulas, Tables, and Specifications
| Rebound (r) | Correction at Horizontal (x=0) |
|---|---|
| 10 | -3.2 |
| 20 | -3.4 |
| 30 | -3.1 |
| 40 | -2.7 |
| 50 | -2.2 |
| 60 | -1.7 |
| Term | Description | Grade |
|---|---|---|
| Fresh | No visible weathering | I |
| Moderately weathered | <50% decomposed/disintegrated | III |
| Highly weathered | >50% decomposed/disintegrated | IV |
| Completely weathered | All decomposed but structure intact | V |
| Residual soil | All converted to soil, structure destroyed | VI |
| Grade | Description | Field ID | UCS Range (MPa) |
|---|---|---|---|
| R0 | Extremely weak rock | Indented by thumb-nail | 0.25 - 1.0 |
| R1 | Very weak rock | Crumbles under hammer blows | 1.0 - 5.0 |
| R2 | Weak rock | Peeled with difficulty by knife | 5.0 - 25 |
| R3 | Medium strong rock | Fract |
IS 11315 Part 5: Data Analysis & Strength Estimation Summary
| Grade | Description | Field ID | Approx. UCS (MPa) |
|---|---|---|---|
| S1-S6 | Very soft to hard clay | Penetration by fist/thumb/nail | <0.025 to >0.50 |
| RO-R6 | Extremely weak to extremely strong rock | Hammer/knife tests | 0.25 to >250 |
If rock is "Medium strong" (R3), fractured by single hammer blow:
UCS ≈ 25-50 MPa
graph LR
A[Rebound Number (r)] --> B[Correct for Orientation]
B --> C[Use Fig. 1 Chart]
C --> D[Estimate UCS (MPa)]
E[Rock Density (γ)] --> C
This process ensures a practical
IS 11315 Part 5 (1987) - Presentation of Results: Key Points
| Term | Description | Grade |
|---|---|---|
| Fresh | No visible weathering; slight discoloration on discontinuities | I |
| Moderately weathered | <50% decomposed/disintegrated; fresh rock present as framework/core stones | III |
| Highly weathered | >50% decomposed/disintegrated; fresh rock discontinuous framework/core stones | IV |
| Completely weathered | All decomposed/disintegrated; original mass structure largely intact | V |
| Residual soil | All converted to soil; structure/fabric destroyed; volume change but soil not transported | VI |
| Term | Description |
|---|---|
| Fresh | No visible weathering |
| Discoloured | Colour changed; specify degree and minerals affected |
| Decomposed | Weathered to soil with intact fabric but mineral grains decomposed |
| Disintegrated | Weathered to soil, friable, fabric intact, mineral grains not decomposed |
| Grade | Description | Field ID | Approx. UCS (MPa) |
|---|---|---|---|
| S1-S6 | Clays (very soft to hard) | Penetration varies (fist/thumb/nail) | <0.5 to >0.5 |
| R0-R6 | Rock (extremely weak to extremely strong) | Indentation and fracturing by hammer/knife | 0.25 to >250 |
IS 11315 Part 5 (1987) - Limitations and Precautions Summary
| Rebound (r) | Vertical Down (-90°) | -45° | Horizontal (0°) | +45° | Vertical Up (+90°) |
|---|---|---|---|---|---|
| 10 | 0 | -0.8 | -3.2 | - | - |
| 20 | 0 | -0.9 | -3.4 | -6.9 | -8.8 |
| 30 | 0 | -0.8 | -3.1 | -6.2 | -7.8 |
| 40 | 0 | -0.7 | -2.7 | -5.3 | -6.6 |
| 50 | 0 | -0.6 | -2.2 | -4.3 | -5.3 |
| 60 | 0 | -0.4 | -1.7 | -3.3 | -4.0 |
| Term | Description | Grade |
|---|---|---|
| Fresh | No visible weathering, slight discoloration only | I |
| Moderately Weathered | <50% decomposed/disintegrated; |
IS 11315 Part 5 (1987) — Key References Summary
| Term | Description | Grade |
|---|---|---|
| Fresh | No visible weathering; slight discoloration on discontinuities | I |
| Moderately weathered | <50% rock decomposed/disintegrated; fresh/discoloured rock as continuous framework/core stones | III |
| Highly weathered | >50% rock decomposed/disintegrated; fresh/discoloured rock discontinuous framework/core stones | IV |
| Completely weathered | All rock decomposed/disintegrated; original mass structure largely intact | V |
| Residual soil | All rock converted to soil; mass structure destroyed; volume change but soil not transported | VI |
| Term | Description |
|---|---|
| Fresh | No visible weathering |
| Discoloured | Colour changed; specify degree and affected minerals |
| Decomposed | Weathered to soil; original fabric intact but mineral grains decomposed |
| Disintegrated | Weathered to soil; fabric intact; friable rock but mineral grains not decomposed |
| Grade | Description | Field ID | Approx. UCS Range (MPa) |
|---|---|---|---|
| S1-S6 | Cohesive soils (clays) | Penetration/indentation by thumb/fist | <0.5 |
| RO-R6 | Rock strength levels | From thumb-nail indent to chipping with hammer | 0.25 to >250 |
| Rebound (r) | -45° | +45° | Horizontal (0°) |
IS 11315 Part 5 (1987) primarily deals with the presentation of results for concrete tests, including annexures and conversion tables.
Annexures typically include:
Conversion Tables cover:
| Quantity | From | To | Factor |
|---|---|---|---|
| Pressure/Stress | psi | MPa | 0.006895 |
| Length | inch | mm | 25.4 |
| Weight | lb | kg | 0.4536 |
| Volume | ft³ | m³ | 0.02832 |
[ f_{c,28} = f_{c,t} \times \frac{f_{c,28,ref}}{f_{c,t,ref}} ]
Where:
For detailed annexures and exact tables, refer to the official IS 11315 Part 5 document.
Frequently Asked
Recommended Procedure for Using Schmidt Hammer on Rock Discontinuity Walls (IS 11315 Part 5):
| Hammer Orientation | Correction to Rebound Number (r) |
|---|---|
| Vertical Downwards | 0 (no correction) |
| Vertical Upwards | Subtract 4 to 9 (varies with r) |
| Horizontal | Subtract ~1.7 to 3.4 (varies) |
| 45° Inclined | Subtract ~0.4 to 6.9 (varies) |
This test estimates Joint Wall Compressive Strength (JCS), critical for shear strength calculations using the Joint Roughness Coefficient (JRC).
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References: IS 11315 Part 5, Clauses 3.6.1, 4.4, 4.4.4, 4.4.5 and Table 4.
According to IS 11315 Part 5, weathering significantly reduces the compressive strength of rock walls, especially at discontinuity surfaces:
| Weathering Grade | Description | Approx. UCS Range (MPa) |
|---|---|---|
| Fresh (I) | No visible weathering | High (>50 MPa typical) |
| Moderately (III) | <50% decomposed/disintegrated | Moderate (5-50 MPa) |
| Highly (IV) | >50% decomposed/disintegrated | Low (1-5 MPa) |
| Completely (V) | Fully decomposed, structure intact | Very low (<1 MPa) |
| Residual Soil (VI) | Rock converted to soil | Very low (<0.5 MPa) |
Note: Weathering reduces rock wall strength mainly by altering discontinuity surfaces, critical for stability assessment.
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Equipment Required for Wall Strength Evaluation as per IS 11315 Part 5 (1987):
Additional Notes:
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This setup ensures comprehensive and representative wall strength assessment as per IS 11315 Part 5.
Conversion of Schmidt Hammer Rebound (r) to Joint Wall Compressive Strength (JCS):
Parameters needed:
Procedure:
Important Notes:
| r (downwards) | At -45° | At +45° | Horizontal (0°) |
|---|---|---|---|
| 10 | -0.8 | - | -3.2 |
| 20 | -0.9 | -6.9 | -3.4 |
| 30 | -0.8 | -6.2 | -3.1 |
| 40 | -0.7 | -5.3 | -2.7 |
| 50 | -0.6 | -4.3 | -2.2 |
| 60 | -0.4 | -3.3 | -1.7 |
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Limitations of Field Testing Methods for Rock Wall Strength in Loose or Heavily Fractured Rock Masses (IS 11315 Part 5):
Discontinuity Dominance: Loose/fractured rock masses behave as discontinuous media; discontinuities largely control mechanical behavior, making direct strength measurement of intact rock less representative.
Thin Wall Skin: The shear strength is governed by a thin "skin" of wall rock or mineral coatings, which is difficult to test accurately by conventional methods.
Sampling Challenges: Manual index tests require hand-sized fresh samples from discontinuity walls; in loose/fractured masses, obtaining representative samples is difficult.
Test Sensitivity: Schmidt hammer and manual index tests estimate apparent strength but may not capture variability due to weathering or alteration states.
Conventional Tests Unsuitable: Standard tests on rock cylinders cannot test thin wall skins or coatings, limiting their applicability.
Interpretation Complexity: Field tests must be combined with careful geological descriptions to reliably interpret results.
| Limitation Aspect | Explanation |
|---|---|
| Discontinuity effects | Strength governed by discontinuities, not intact rock |
| Thin wall skin | Difficult to test thin, weathered coatings accurately |
| Sampling representativeness | Hard to get fresh, representative samples in loose/fractured rock |
| Test method sensitivity | Index tests provide approximate strength only |
| Conventional test limits | Cannot test thin wall rock or coatings |
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In essence: Field tests in such rock masses provide approximate strength values and must be supplemented by detailed geological assessment for reliable design.
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