IS 11315 Part 101987AI Search Enabled✦ AI Generated

Method for the quantitative description of discontinuities in rock masses, Part 10: Block size

IS 11315 Part 10 (1987) specifies a standardized method for quantitatively describing the size and shape of blocks formed by intersecting discontinuities in rock masses. It provides engineers and geologists with a systematic approach to assess block dimensions based on joint spacing, number of joint sets, and their persistence, which are critical for understanding rock mass behavior in engineering projects such as tunneling, slope stability, and foundation design.

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1987Edition
Rock MechanicsCategory
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What This Standard Covers

IS 11315 Part 10 (1987) specifies a standardized method for quantitatively describing the size and shape of blocks formed by intersecting discontinuities in rock masses. It provides engineers and geologists with a systematic approach to assess block dimensions based on joint spacing, number of joint sets, and their persistence, which are critical for understanding rock mass behavior in engineering projects such as tunneling, slope stability, and foundation design.

Who Uses This Standard

  • Geotechnical Engineers
  • Rock Mechanics Specialists
  • Mining Engineers
  • Civil Engineers
  • Geologists
  • Structural Engineers
  • Tunnel and Slope Stability Analysts

Key Topics Covered

Definition and significance of block size in rock masses
Influence of discontinuity spacing and number of joint sets
Quantitative measurement of block size index (Ip)
Volumetric joint count and joint spacing measurement methods
Classification of block shapes and descriptions
Effect of block size on mechanical behavior of rock masses
Field procedures for recording discontinuities
Interpretation of blockiness in rock mass characterization
Guidelines for sampling lengths and joint counting
Reporting and rounding off numerical values
Relationship between block size and rock mass strength
Use of modal block size indices for different rock domains

Table of Contents

1Scope

IS 11315 Part 10 - Scope Summary

  • Scope Reference: IS 11315 Part 10 refers to definitions and terms as per IS 11358-1986.
  • Purpose: Specifies testing and analysis procedures related to the material or product covered.
  • Rounding Off: Final test results must be rounded according to IS 2-1960 (Rules for rounding off numerical values).

Key Points:

  • No direct formulas or tables are provided in the Scope clause.
  • Definitions and terminologies are governed by IS 11358-1986.
  • Reporting and rounding of values must comply with IS 2-1960.

Additional Notes (General Practice):

  • Always refer to IS 11358-1986 for term definitions.
  • Follow IS 2-1960 for rounding:
    • If the digit after the last significant figure is >5, round up.
    • If <5, round down.
    • If exactly 5, round to the nearest even digit.
flowchart LR
  A[IS 11315 Part 10] --> B[Definitions per IS 11358-1986]
  A --> C[Rounding per IS 2-1960]

For detailed formulas or tables, consult respective parts of IS 11315 or related IS codes.

2Definitions

IS 11315 Part 10: Definitions & Key Specifications

  • Definitions:
    As per Clause 2.1, definitions follow IS 11358-1986 (general rock mass terminology).

  • Block Size Classification (Clause 4.3):
    Based on Jv (joints per m³), which quantifies block size via joint density:

DescriptionJv (joints/m³)
Very large blocks< 1.0
Large blocks1 - 3
Medium-sized blocks3 - 10
Small blocks10 - 30
Very small blocks> 30
  • Additional Note:
    • Jv > 60 indicates crushed rock, typical of a clay-free crushed zone.

Summary

  • Use Jv to classify rock block sizes.
  • Refer to IS 11358-1986 for detailed terminology.
  • This classification aids in rock mass characterization for design and analysis.
flowchart TD
    A[Joint Density (Jv)] --> B{Jv Value}
    B -->|<1| C[Very Large Blocks]
    B -->|1-3| D[Large Blocks]
    B -->|3-10| E[Medium-sized Blocks]
    B -->|10-30| F[Small Blocks]
    B -->|>30| G[Very Small Blocks]
    B -->|>60| H[Crushed Rock Zone]
3Significance of Block Size in Rock Mass Behaviour

Significance of Block Size in Rock Mass Behaviour (IS 11315 Part 10)

  • Block Size Definition (Clause 3.1):
    Determined by discontinuity spacing, number of joint sets, and persistence of discontinuities.

  • Mechanical Behaviour (Clause 3.3):

    • Large blocks → less deformable rock mass, favorable arching & interlocking in underground works.
    • Small blocks → soil-like behaviour; failure modes shift from translational/toppling to circular/rotational.
    • Extremely small blocks → may behave like a flow zone (e.g., "sugar-cube" shear zone).
  • Quantitative Measures (Clause 3.5):

    • Block Size Index (Ib): Average dimension of typical blocks.
    • Volumetric Joint Count (Jv): Total number of joints per unit volume.

Key Formulas

  • Volumetric Joint Count (Jv):

    [ J_v = \sum_{i=1}^{n} \frac{1}{S_i} ]

    where:
    ( S_i ) = mean spacing of joints in the ( i^{th} ) set
    ( n ) = number of joint sets

  • Block Size Index (Ib):
    Approximate average block dimension, inversely proportional to ( J_v ):

    [ I_b \approx \frac{1}{J_v} ]


Summary Table

ParameterDescriptionEffect on Rock Mass Behaviour
Block Size Index (Ib)Average block dimensionLarger Ib → stiffer rock mass
Volumetric Joint Count (Jv)Number of joints per unit volumeHigher Jv → smaller block size, more deformable
flowchart LR
    A[Discontinuity Spacing & Sets] --> B[Block Size (Ib)]
    B --> C[Rock Mass Behaviour]
    C --> D{Block Size}
    D -->|Large| E[Less deformable, arching]
    D -->|Small| F[Soil-like failure modes]
    D -->|Very Small| G[Flow-like behaviour]

In essence: Block size critically controls deformation and failure modes in rock masses,

4Field Measurement and Quantitative Description

IS 11315 Part 10 focuses on quantitative description of block size and shape formed by intersecting discontinuities in rock masses.

Key Points & Formulas:

  • Block Size Measurement:

    • Blocks are characterized by their linear dimensions (length, width, height) measured along discontinuity intersections.
    • The mean block size (L) is often taken as the average of these dimensions.
  • Block Shape Description:

    • Shape is described by ratios of block dimensions:
      • Shape Ratio 1: ( \frac{L_{min}}{L_{max}} )
      • Shape Ratio 2: ( \frac{L_{mid}}{L_{max}} )
    • These ratios help classify blocks as cubic, tabular, or elongated.
  • Quantification Method:

    • Measure block sizes in the field using tape or laser distance meters.
    • Record multiple blocks for statistical reliability.
    • Calculate average block size and shape ratios.

Typical Table Format for Block Size:

Block No.Length (L_max)Width (L_mid)Height (L_min)Shape Ratio 1Shape Ratio 2
12.5 m2.0 m1.8 m0.720.80
23.0 m2.5 m2.0 m0.670.83
..................

Summary:

  • Measure block dimensions along discontinuity intersections.
  • Calculate shape ratios for block shape classification.
  • Use statistical averages for engineering design inputs.
flowchart TD
    A[Field Measurement] --> B[Measure Block Dimensions]
    B --> C[Calculate Mean Block Size]
    B --> D[Calculate Shape Ratios]
    C --> E[Quantitative Description]
    D --> E

This method ensures consistent, quantitative characterization of rock blocks per IS 11315 Part 10.

5Recording and Reporting Block Size Indices

IS 11315 Part 10: Recording and Reporting Block Size Indices

Key Formulas and Specifications

  • Block Size Index (Ib):
    Estimated by averaging typical block dimensions selected visually.

    • Accuracy: ±10% is sufficient.
    • Purpose: Represents average block dimensions realistically.
  • Formula for Sedimentary Rocks (3 sets of joints):
    [ I_b = \frac{S_1 + S_2 + S_3}{3} ]
    where (S_1, S_2, S_3) = modal spacings of joint sets.

  • Important Notes:

    • For >3 joint sets, averaging spacings can overestimate (I_b) due to widely spaced sets.
    • Record the modal block size index (I_p) for largest, smallest blocks and domain details (number of sets, persistence).

Data to Record (Clause 5.1)

  • Modal block size index (I_p) (typical, largest, smallest)
  • Number of joint sets
  • Persistence and description of joints

Summary Table

ParameterDescriptionNotes
(I_b)Average block size index±10% accuracy
(S_1, S_2, S_3)Modal spacings of joint setsUse for sedimentary rocks
(I_p)Modal block size index for reportingRecord for domain sizes
Number of setsNumber of joint setsDescribe persistence
flowchart TD
    A[Select typical block sizes] --> B[Measure average dimensions (Ib)]
    B --> C{Number of joint sets > 3?}
    C -- Yes --> D[Use caution; wide sets may skew Ib]
    C -- No --> E[Calculate Ib = (S1 + S2 + S3)/3]
    E --> F[Record Ip (modal block size indices)]
    D --> F
    F --> G[Report number of sets and persistence]

This approach ensures realistic block size representation for engineering and geological assessments.

6Classification of Rock Mass Blockiness

IS 11315 Part 10: Classification of Rock Mass Blockiness

Key Formulas:

  • Block Size Index (Ib):
    Average dimension of typical rock blocks, estimated visually with ~10% accuracy.
    For multiple joint sets (especially 3 or more):
    [ I_b = \frac{S_1 + S_2 + S_3}{3} ]
    where (S_1, S_2, S_3) = average spacings of the three principal joint sets.

Classification Terms (Clause 5.3 & 4.4):

DescriptionCharacteristics
MassiveFew joints, very wide spacing, equidimensional blocks
BlockyBlocks formed by multiple joint sets, roughly equidimensional
TabularOne dimension much smaller than the other two (plate-like)
ColumnarOne dimension much larger than the other two (pillar-like)
CrushedVery closely spaced joints, resembling "sugar cube" blocks

Notes:

  • Avoid using average modal spacings if more than three joint sets exist, as widely spaced sets can skew (I_b).
  • Sedimentary rocks commonly have cubic/prismatic blocks due to two cross joints plus bedding planes.
flowchart LR
    A[Rock Mass] --> B{Blockiness Type}
    B --> C[Massive]
    B --> D[Blocky]
    B --> E[Tabular]
    B --> F[Columnar]
    B --> G[Crushed]

This classification aids in understanding rock stability and excavation behavior.

7Notes on Joint Sets and Sampling Procedures

IS 11315 Part 10: Notes on Joint Sets and Sampling Procedures

Key Points & Formulas

  • Sampling length: Use 5 or 10 m perpendicular to joint sets for counting joints (Clause 4.2.1).
  • Joint count per metre:
    [ \text{Joint count per metre} = \frac{\text{Number of joints counted}}{\text{Sampling length (m)}} ]
  • Volumetric Joint Count (Jv): Sum of joints per metre for all joint sets present (Clause 4.2).
    [ J_v = \sum \text{(joints per metre for each set)} ]
  • Random discontinuities can be included but usually have minimal effect unless systematic joint spacing is wide (1-10 m).

Block Size Classification (Clause 4.3)

Description( J_v ) (joints/m³)
Very large blocks< 1.0
Large blocks1 - 3
Medium-sized blocks3 - 10
Small blocks10 - 30
Very small blocks> 30
  • Note: ( J_v > 60 ) indicates crushed rock (clay-free crushed zone).

Sampling Procedure Summary

  • Face the direction of strike for each joint set.
  • Count joints perpendicular to strike to avoid angular corrections.
  • Use paced or estimated lengths (±10% accuracy).
  • Use mean spacing, not modal spacing, for calculations.
flowchart TD
    A[Select Joint Set] --> B[Face Direction of Strike]
    B --> C[Count Joints Perpendicular to Strike]
    C --> D[Divide Count by Sampling Length (5 or 10 m)]
    D --> E[Calculate Jv = Sum of Joints/m for all Sets]
    E --> F[Classify Block Size based on Jv]

This ensures rapid, reliable field mapping and block size estimation.

8Application Guidelines

IS 11315 Part 10 (1987) - Application Guidelines: Key Points

IS 11315 Part 10 refers to prestressed concrete, and its application guidelines align with IS 11358-1986 definitions.

Key Specifications & Formulas

  • Prestressing Force (P):
    [ P = A_p \times f_{pu} ]
    Where:

    • (A_p) = Area of prestressing steel
    • (f_{pu}) = Ultimate tensile strength of prestressing steel
  • Losses in Prestress:
    Consider initial prestress force minus losses due to:

    • Elastic shortening
    • Creep and shrinkage of concrete
    • Relaxation of steel
    • Anchorage slip
  • Allowable Stresses:
    Follow limits as per IS 1343 for concrete and prestressing steel.

Tables (Typical)

ParameterTypical Value / Range
Ultimate tensile strength (f_{pu})1100 - 1860 MPa
Modulus of elasticity of steel (E_p)195 - 210 GPa
Permissible stress in concrete (compression)As per IS 456 guidelines

Application Notes

  • Use IS 11358 for term definitions and IS 1343 for prestressed concrete design.
  • Ensure proper anchorage and stress transfer.
  • Account for all prestress losses in design calculations.
flowchart LR
    A[Prestressing Steel Area \(A_p\)] --> B[Calculate Initial Force \(P\)]
    B --> C[Subtract Losses]
    C --> D[Effective Prestress Force]
    D --> E[Check Against Allowable Stresses]

For detailed design, always cross-reference IS 1343 and IS 11358 along with IS 11315 Part 10.

9Rounding Off Numerical Values

Rounding Off Numerical Values as per IS 11315 Part 10

  • Reference Standard: IS 11315 Part 10 mandates rounding off numerical results according to IS 2:1960 (Rules for rounding off numerical values).

Key Points from IS 2:1960 (Rounding Rules)

ConditionRuleExample
If the digit to be dropped < 5Leave the last retained digit unchanged3.142 → 3.14
If the digit to be dropped > 5Increase the last retained digit by 13.146 → 3.15
If the digit to be dropped = 5 followed by non-zero digitsIncrease the last retained digit by 13.1451 → 3.15
If the digit to be dropped = 5 and no following digitsIncrease last digit if odd, else leave unchanged (round half to even)3.145 → 3.14 (if last digit 4 is even) or 3.135 → 3.14 (if last digit 3 is odd)

Summary

  • Always round off final test or analysis results in accordance with IS 2:1960.
  • This ensures uniformity and accuracy in reporting.
  • No specific rounding rules are detailed in IS 11315 Part 10 except this reference.

flowchart TD
    A[Final Value] --> B{Digit to be dropped}
    B -->|<5| C[Leave last digit unchanged]
    B -->|>5| D[Increase last digit by 1]
    B -->|=5 followed by non-zero| D
    B -->|=5 no following digits| E{Is last digit odd?}
    E -->|Yes| D
    E -->|No| C

Use IS 2:1960 for consistent rounding in rock mechanics test results per IS 11315 Part 10.

10References and Related Standards

IS 11315 Part 10 (1987) - References and Related Standards

  • Primary Reference:

    • Definitions and terms are as per IS 11358-1986 (Terminology related to the standard).
  • Rounding Off Results:

    • Follow IS 2-1960 for rounding off numerical values in test reports.
    • Typically, rounding is done to a specified number of decimal places based on measurement precision.
  • Related Standards:

    • IS 11315 series covers various test methods; Part 10 refers to specific procedures within this series.
    • IS 11358-1986 provides fundamental definitions ensuring consistency across tests.

Summary Table of References

IS CodePurposeNotes
IS 11358-1986Definitions and TerminologyApplies to IS 11315 series
IS 2-1960Rules for Rounding Off NumbersUsed for reporting test results
IS 11315 (Part 10)Specific test method standard1987 version

If you need formulas or tables for a specific test in IS 11315 Part 10, please specify the test type for detailed data.

Popular Questions About IS 11315 Part 10

?How is block size quantitatively determined according to IS 11315 Part 10?

According to IS 11315 Part 10 (1987), block size in rock masses is quantitatively determined as follows:

  • Definition: Block size describes the shape and dimensions of rock blocks formed by intersecting discontinuity sets (joints, bedding, cleavage).
  • Measurement: Use a tape of at least 3 m length, calibrated in millimeter divisions.
  • Procedure: Measure the dimensions of the block formed at the intersection of discontinuities directly in the field.
  • The block size reflects the mutual orientation of discontinuity sets, i.e., the spatial geometry controls block dimensions.

Summary:

ParameterDescription
Tape lengthMinimum 3 meters
CalibrationMillimeter divisions
Block size basisIntersection geometry of discontinuities

This method provides a quantitative, field-based measurement of rock block sizes for engineering and rock mechanics analysis.

?What role do joint sets and their persistence play in defining block size?

Role of Joint Sets and Persistence in Defining Block Size (IS 11315 Part 10):

  • Joint Sets: The number and mutual orientation of joint (discontinuity) sets control the shape and size of rock blocks. Intersecting joint sets form the boundaries of blocks.
  • Persistence: Persistence refers to the extent or length of individual discontinuities. Longer, continuous joints create larger, well-defined blocks, while short or discontinuous joints lead to smaller or irregular blocks.
  • Block Size Determination:
    • Block size depends on discontinuity spacing, number of joint sets, and persistence of these joints (Clause 3.1).
    • The block size is measured physically using a tape (≥3 m) (Clause 3.6).
    • It can be quantified by:
      • Block Size Index (Ib): Average dimension of typical blocks.
      • Volumetric Joint Count (Jv): Total number of joints intersecting a unit volume (Clause 3.5).
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Summary: Joint sets define block boundaries via their orientation and number; persistence controls block continuity, both crucial for block size and rock mass behavior.

?How should volumetric joint count be measured and applied in the field?

Volumetric Joint Count (Jv) Measurement & Application (IS 11315 Part 10)

  • Definition:
    Jv = sum of joints per metre for each joint set present (Clause 4.2).

  • Field Measurement Procedure:

    • Pace out or estimate a 5 or 10 m sampling length perpendicular to the strike of each joint set (Clause 4.2, 4.2.1).
    • Count the number of joints intersecting this length for each joint set.
    • Divide the count by the sampling length to get joints per metre.
    • Sum these values for all joint sets to get Jv.
    • Random discontinuities may be included but generally have minimal effect unless systematic joint spacing is wide (1–10 m) (Clause 4.2 Notes).
  • Important Notes:

    • Face in the direction of strike to avoid angular corrections (Clause 4.2 Note 1).
    • Use mean spacing, not modal spacing, for calculations (Clause 4.2 Note 2).
    • Record Jv along with the number of joint sets and their persistence (Clause 5.2).

Formula Summary:

[ J_v = \sum_{i=1}^{n} \frac{\text{Number of joints in set } i}{\text{Sampling length (m)}} ]

Where:

  • (n) = number of joint sets
  • Sampling length = 5 or 10 m (recommended)

Visual Concept:

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This method ensures rapid, reliable estimation of joint density for rock mass characterization.

?What are the typical block shape classifications described in this standard?

According to IS 11315 Part 10 (1987), typical block shape classifications for rock masses are:

  • Massive: Few joints, very wide spacing; blocks are approximately equidimensional.
  • Blocky: Blocks formed by multiple joint sets; shape varies but generally equidimensional.
  • Tabular: One dimension is considerably smaller than the other two, forming plate-like blocks.
  • Columnar: One dimension is considerably larger than the other two, forming column-like blocks.
  • Crushed: Heavily jointed, blocks resemble "sugar cubes" due to intense fragmentation.

These shapes result from the number and orientation of joint sets, with sedimentary rocks often producing more regular shapes like cubes or rhombohedrons.

Visual representation (Fig. 1 in the standard) is recommended for clarity, showing typical block shapes and sizes.

Loading diagram...

This classification aids in understanding rock mass behavior and stability.

?How does block size influence the mechanical behavior and stability of rock masses?

Influence of Block Size on Rock Mass Mechanical Behavior and Stability (IS 11315 Part 10)

  • Block Size Definition: Determined by discontinuity spacing, number of sets, and persistence (Clauses 3.1, 3.6).
  • Mechanical Behavior:
    • Large blocks → Less deformable rock mass.
    • Large blocks favor arching and interlocking, enhancing underground stability (Clause 3.3).
    • Small blocks → Behavior closer to soil, with circular/rotational failure modes typical of soils rather than rock (Clause 3.3).
    • Extremely small blocks may behave like a flowing shear zone (e.g., quartzite sugar-cube shear zone).
  • Stability Implications:
    • Large blocks promote translational/toppling failures.
    • Small blocks increase potential for soil-like failures.

Measurement: Block size is measured using a tape ≥ 3 m with mm accuracy (Clause 3.6).

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Summary: Block size critically controls rock mass stiffness, failure mode, and stability, influencing engineering design and risk assessment.

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