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Glossary of terms and symbols relating to rock mechanics

IS 11358:1987 provides a comprehensive glossary of terms and symbols used in rock mechanics, essential for understanding and communicating concepts related to rock properties, behaviors, and engineering applications. This standard is crucial for geotechnical engineers, mining engineers, and researchers working with rock mass characterization, tunnel construction, and underground excavations.

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1987Edition
Rock MechanicsCategory
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What This Standard Covers

IS 11358:1987 provides a comprehensive glossary of terms and symbols used in rock mechanics, essential for understanding and communicating concepts related to rock properties, behaviors, and engineering applications. This standard is crucial for geotechnical engineers, mining engineers, and researchers working with rock mass characterization, tunnel construction, and underground excavations.

Who Uses This Standard

  • Geotechnical Engineers
  • Mining Engineers
  • Civil Engineers
  • Rock Mechanics Researchers
  • Tunnel Designers
  • Geologists
  • Construction Managers

Key Topics Covered

Rock density and dry density
Deformation and elastic moduli
Rock mass behavior under stress
Rock discontinuities and joint characteristics
Blasting techniques and controlled blasting
Rock pressure and squeezing ground conditions
Rock failure modes including rock bursts and fatigue
Hydraulic fracturing and borehole definitions
Rock weathering and durability indices
Stress representation and stress ellipsoids
Shotcrete application and tunnel support
Rock mass classification and drilling conditions

Table of Contents

1Scope

IS 11358: Scope Summary

IS 11358 covers definitions, terms, and symbols related to rock mechanics. It standardizes the vocabulary used in rock mechanics engineering, ensuring uniform communication.

Key Points from Scope:

  • Applies to rock mechanics terminology.
  • Covers definitions related to rock properties, testing, and behavior.
  • Includes symbols used in rock engineering calculations.

Important Specifications:

  • No direct formulas or tables in the scope clause.
  • Serves as a reference glossary for other IS codes involving rock mechanics.

Typical Symbols & Terms (examples):

SymbolMeaning
σStress
εStrain
EModulus of Elasticity
UCSUniaxial Compressive Strength

Usage:

  • Refer IS 11358 for standardized terms when designing or analyzing rock structures.
  • Use alongside IS codes on rock testing and design (e.g., IS 6928).
flowchart LR
    A[IS 11358] --> B[Glossary of Terms]
    A --> C[Symbols for Rock Mechanics]
    B --> D[Rock Properties]
    C --> D
    D --> E[Design & Analysis]

For detailed formulas and tables, consult related IS codes on rock testing and design.

2Definitions of Terms and Symbols

IS 11358: Definitions of Terms and Symbols in Rock Mechanics

IS 11358 primarily provides a glossary of standardized terms and symbols used in rock mechanics, ensuring uniformity in communication rather than formulas or tables.

Key Highlights:

  • Scope: Defines terminology related to rock properties, behavior, and testing.
  • Symbols: Standard symbols for parameters like:
    • σ = Stress
    • ε = Strain
    • E = Modulus of Elasticity
    • c = Cohesion
    • φ = Angle of internal friction
    • γ = Unit weight
  • Terms: Includes definitions of rock mass, discontinuities, joint sets, rock strength, deformability, and failure criteria.

Typical Parameters Defined:

SymbolMeaningUnit
σStressMPa or kN/m²
εStrainDimensionless
EElastic modulusMPa
cCohesionMPa
φAngle of internal frictionDegrees
γUnit weightkN/m³

Usage:

  • Use these terms and symbols consistently in rock mechanics analysis, reporting, and design.
  • Refer to IS 11358 for exact definitions to avoid ambiguity.
flowchart LR
    A[Rock Mechanics] --> B[Terminology]
    A --> C[Symbols]
    B --> D[Rock Mass]
    B --> E[Discontinuities]
    C --> F[Stress (σ)]
    C --> G[Strain (ε)]
    C --> H[Modulus of Elasticity (E)]

Note: For detailed formulas and testing procedures, refer to complementary IS codes like IS 11282 (rock testing) or IS 14687 (rock slopes).

3Rock Properties and Parameters

IS 11358: Key Rock Properties & Parameters

The standard emphasizes a Basic Geotechnical Description (BGD) of rock mass using five key parameters (Clause 2.22):

ParameterDescriptionSymbol Example
Rock Name (Geology)Geological classificationQuartz
Layer ThicknessThickness of rock layerL2 (Layer 2)
Fracture InterceptFrequency or spacing of fracturesF4 (Fracture 4)
Uniaxial Compressive Strength (UCS)Rock strength under compressionS3 (Strength 3)
Angle of Friction of FracturesShear strength parameterA2 (Angle 2)

Hydraulic Conductivity (K) (Clause 2.148) defines permeability of rock mass to water, crucial for seepage and drainage analysis.


Typical UCS Classification (for reference):

UCS (MPa)Rock Strength Category
> 250Very Strong
100 - 250Strong
50 - 100Medium
25 - 50Weak
< 25Very Weak

Summary Diagram of BGD Parameters:

graph LR
A[Rock Mass] --> B[Rock Name (Geology)]
A --> C[Layer Thickness (L)]
A --> D[Fracture Intercept (F)]
A --> E[UCS (S)]
A --> F[Angle of Friction (A)]
A --> G[Hydraulic Conductivity (K)]

Use these parameters for consistent rock mass characterization per IS 11358.

4Rock Mass Behavior and Deformation

IS 11358 focuses on terminology and basic parameters for rock mechanics but lacks detailed formulas on rock mass behavior and deformation. Based on standard rock mechanics principles, here are key points:

Key Parameters (from Clause 2.22)

  • Rock Name (Geological description)
  • Layer Thickness (L)
  • Fracture Intercept (F)
  • Uniaxial Compressive Strength (σ_c)
  • Angle of Friction of Fractures (φ)

Typical Formulas for Rock Mass Behavior

  1. Deformation Modulus (E_rm) of Rock Mass
    Empirical relation (Hoek & Brown): [ E_{rm} = 5000 \times \text{GSI} \times \left(\frac{\sigma_c}{100}\right) ] where GSI = Geological Strength Index.

  2. Hoek-Brown Failure Criterion
    [ \sigma_1 = \sigma_3 + \sigma_c \left(m_b \frac{\sigma_3}{\sigma_c} + s \right)^a ]

    • ( \sigma_1, \sigma_3 ) = major and minor principal stresses
    • ( m_b, s, a ) = constants based on rock mass quality
  3. Hydraulic Conductivity (K)
    From Clause 2.148, permeability is key for fluid flow analysis.

Typical Table: Rock Mass Quality (GSI)

GSI ValueRock Mass DescriptionExpected Behavior
80-100Very Good RockHigh strength, low deformation
40-60Fair RockModerate strength and deformation
< 40Poor RockLow strength, high deformation

flowchart LR
    A[Rock Mass Parameters] --> B[Geological Description]
    A --> C[Layer Thickness (L)]
    A --> D[Fracture Intercept (F)]
    A --> E[Uniaxial Compressive Strength (σ_c)]
    A --> F[Angle of Friction (φ)]
    B & C & D & E & F --> G[Rock Mass Behavior & Deformation]

Summary: Use rock mass parameters to estimate deformation modulus and strength via Ho

5Rock Discontinuities and Structural Features

IS 11358 Key Parameters for Rock Discontinuities & Structural Features

The code defines 10 essential parameters describing discontinuities in rock masses:

ParameterDescription
OrientationDip direction (azimuth) & dip angle of discontinuity plane
SpacingMean perpendicular distance between adjacent discontinuities
PersistenceTrace length of discontinuity; extent in rock mass
RoughnessSurface texture affecting shear strength; includes waviness
Wall StrengthCompressive strength of rock walls adjacent to discontinuity
AperturePerpendicular opening width between rock walls (air/water filled)
FillingMaterial between walls (e.g., clay, silt, gouge), usually weaker than rock
SeepagePresence of water flow/moisture in discontinuities
Number of SetsNumber of intersecting joint sets
Block SizeDimensions of rock blocks formed by intersecting discontinuities

Important Notes:

  • Shear Strength of Discontinuity depends on roughness, wall strength, filling, and aperture.
  • Block Size influences stability and excavation design.
  • Orientation and spacing govern rock mass anisotropy and strength.

Typical Formula for Shear Strength (Coulomb Criterion):

[ \tau = c + \sigma_n \tan \phi ]

Where:

  • (\tau) = shear strength of discontinuity
  • (c) = cohesion (depends on filling and wall strength)
  • (\sigma_n) = normal stress on discontinuity
  • (\phi) = friction angle (affected by roughness and filling)

graph TD
A[Rock Mass] --> B[Discontinuities]
B --> C[Orientation]
B --> D[Spacing]
B --> E[Persistence]
B --> F[Roughness]
B --> G[Wall Strength]
B --> H[Aperture]
B --> I[Filling]
B --> J[Seepage]
B --> K[Number of Sets]
B --> L[Block Size]

This framework aids in rock mass classification, stability analysis, and design of rock structures per IS 11358.

6Blasting and Excavation Terms

IS 11358: Blasting and Excavation Key Terms & Concepts

  • Blastability (Clause 2.31):

    • Definition: Index representing rock resistance to blasting.
    • Use: Helps select explosive type and charge.
  • Bench Blasting (Clause 2.28):

    • Definition: Excavation in steps (benches) with blast holes drilled parallel to the free face.
    • Application: Common in quarries/open pits for controlled rock breakage.

Typical Parameters & Formulas (General Rock Mechanics Context)

ParameterSymbolTypical UnitNotes
Burden (distance between holes)BmDepends on rock type & explosive
Spacing (between rows)SmUsually 1.2 to 1.5 × Burden
Bench HeightHmHeight of each excavation step
Powder Factor (Explosive per volume)PFkg/m³PF = Explosive weight / Rock volume

Basic formula for explosive charge per hole:
[ Q = B \times S \times H \times \rho_r \times PF ]
Where:

  • ( Q ) = Explosive charge per hole (kg)
  • ( \rho_r ) = Rock density (kg/m³)

Conceptual Diagram: Bench Blasting Layout

graph TD
    A[Free Face] --> B[Bench 1]
    B --> C[Bench 2]
    C --> D[Bench 3]
    subgraph Blast Holes
        B --> E[Row 1 Holes]
        B --> F[Row 2 Holes]
    end

Note: IS 11358 primarily defines terms; detailed blasting design parameters are found in IS 6922 and IS 8168.

7Rock Pressure and Ground Conditions

IS 11358: Rock Pressure and Ground Conditions

Key Definitions (Clauses)

  • Long-Term Rock Pressure (2.181): Ultimate rock pressure acting on underground supports over time.
  • Horizontal Rock Pressure (2.146): Pressure exerted horizontally on tunnel supports.
  • Vertical Rock Pressure (2.254): Pressure exerted vertically on tunnel supports.

Important Formulas

  1. Vertical Rock Pressure, ( P_v ):
    [ P_v = \gamma \times H ]
    Where:

    • ( \gamma ) = Unit weight of rock (kN/m³)
    • ( H ) = Depth of tunnel (m)
  2. Horizontal Rock Pressure, ( P_h ):
    [ P_h = K \times P_v ]
    Where:

    • ( K ) = Lateral earth pressure coefficient (depends on rock mass properties, typically 0.3 to 1.0)

Typical Values for ( K ) (Lateral Pressure Coefficient)

Rock Condition( K ) Value Range
Intact rock0.3 – 0.5
Jointed rock0.5 – 0.8
Faulted/Weak rock0.8 – 1.0

Notes:

  • Long-term rock pressure accounts for creep and time-dependent deformation.
  • Rock pressure values guide tunnel lining and support design.
flowchart LR
    A[Depth H] --> B[Calculate Vertical Pressure \(P_v = \gamma H\)]
    B --> C[Apply Lateral Coefficient K]
    C --> D[Calculate Horizontal Pressure \(P_h = K P_v\)]
    D --> E[Design Tunnel Supports]

Use these values and formulas as a baseline; adjust based on site-specific investigations and IS 11358 guidelines.

8Failure Modes and Rock Stability

IS 11358 mainly provides glossary and definitions in rock mechanics, not detailed design formulas or tables for failure modes and rock stability.

Key Concepts on Failure Modes (from IS 11358 & general rock mechanics):

  • Shear Failure (Clause 2.276): Movement caused by shear stresses exceeding rock shear strength.
  • Other common failure modes (general knowledge):
    • Tensile failure
    • Compressive failure
    • Sliding failure along discontinuities
    • Toppling failure

Common Rock Stability Checks (beyond IS 11358):

Failure ModeKey ParametersTypical Formula/Criteria
Shear FailureShear strength (τ), Normal stress (σ)Mohr-Coulomb: τ = c + σ tan φ
Sliding FailureFactor of Safety (F_s)F_s = Shear Strength / Shear Stress
Toppling FailureOverturning moment vs. resisting momentStability if resisting moment > overturning moment

Typical Parameters:

  • c = Cohesion of rock
  • φ = Angle of internal friction
  • σ = Normal stress on failure plane

Summary:

  • IS 11358 defines terms like shear failure but does not provide design tables or formulas.
  • For rock stability, use Mohr-Coulomb criterion and factor of safety calculations.
  • Refer to IS 6922 or IS 9456 for detailed rock slope stability design.
flowchart TD
    A[Rock Mass] --> B{Stress Applied}
    B -->|Shear Stress > Shear Strength| C[Shear Failure]
    B -->|Normal Stress + Shear Stress| D[Sliding Failure]
    B -->|Overturning Moment > Resisting Moment| E[Toppling Failure]

For detailed design, consult specific codes like IS 6922 or rock mechanics manuals.

9Hydraulic and Mechanical Testing Terms

IS 11358 primarily provides definitions and symbols related to rock mechanics, including hydraulic and mechanical testing terms, but does not include detailed formulas or tables.

Key Points on Hydraulic and Mechanical Testing Terms in Rock Mechanics (IS 11358):

  • Hydraulic Testing Terms: Include permeability, porosity, pore pressure, hydraulic conductivity.
  • Mechanical Testing Terms: Include uniaxial compressive strength, tensile strength, modulus of elasticity, Poisson’s ratio.

Commonly Used Formulas (from general rock mechanics knowledge):

ParameterFormula
Uniaxial Compressive Strength (UCS)( \sigma_c = \frac{P}{A} ) where (P) = load, (A) = cross-sectional area
Modulus of Elasticity (E)( E = \frac{\sigma}{\epsilon} ) (stress/strain)
Poisson’s Ratio ((\nu))( \nu = -\frac{\epsilon_{trans}}{\epsilon_{axial}} )
Permeability (k)Darcy’s law: ( Q = \frac{k A \Delta h}{\mu L} ) where (Q)=flow rate

Typical Symbols:

  • ( \sigma ): Stress (MPa)
  • ( \epsilon ): Strain (dimensionless)
  • ( k ): Permeability (m/s)
  • ( P ): Load (N)
  • ( A ): Area (m²)

For detailed testing procedures and numerical values, refer to IS 2809 (under revision) or other rock mechanics standards.

flowchart TD
    A[Rock Sample] --> B[Mechanical Testing]
    A --> C[Hydraulic Testing]
    B --> D[UCS, Tensile Strength, Modulus]
    C --> E[Permeability, Porosity, Pore Pressure]
10Support and Protection Methods

IS 11358: Support and Protection Methods - Key Points

1. Support Types (Clause 2.334)

  • Stiff Supports:

    • Minimal deflection under rock pressure
    • Examples: Concrete linings, heavy steel sections
    • Function: Provide rigid confinement
  • Flexible Supports:

    • Significant deflection with rock pressure
    • Examples: Thin steel sections with gravel packing, shotcrete
    • Function: Dissipate strain energy via controlled deformation

2. Yielding Supports (Clause 2.351)

  • Designed to undergo substantial deformation
  • Modify stress distribution around supports
  • Useful in squeezing ground conditions

3. Support Definition (Clause 2.316)

  • Structural elements maintaining underground opening stability

4. Unsupported Span (Clause 2.340)

  • Distance between excavation face and first support or opening width (whichever is less)
  • Critical for stand-up time (time before collapse without support)

Typical Design Considerations:

ParameterNotes
Unsupported SpanMinimize to increase stand-up time
Support TypeChoose based on rock behavior & deformation
Yielding CapacityEnsure supports can deform without failure

flowchart LR
    ExcavationFace -->|Unsupported Span| FirstSupport
    FirstSupport -->|Support Type| StiffSupport & FlexibleSupport
    FlexibleSupport -->|Deforms| EnergyDissipation
    StiffSupport -->|Rigid| RockConfinement
    YieldingSupport -->|Deforms| StressRedistribution

Summary: Select support type based on rock behavior; stiff supports for stable rock, flexible/yielding supports for squeezing or deforming rock. Control unsupported span to ensure stability.

11Stress and Strain Representations

IS 11358: Stress and Strain Representations

Key Concepts

  • Strain Ellipsoid (Clause 2.305):
    Represents strain by deforming a unit sphere into an ellipsoid.

    • Axes = Principal strains (\varepsilon_1, \varepsilon_2, \varepsilon_3)
    • Shows directional strain magnitudes.
  • Stress Ellipsoid (Clause 2.312):
    Represents stress state as an ellipsoid with semi-axes proportional to principal stresses (\sigma_1, \sigma_2, \sigma_3).

    • Axes align with principal stress directions.
    • Coordinates on ellipsoid relate to stress components on planes normal to direction vectors.
  • Young's Modulus (E) (Clauses 2.193 & 2.352):
    Axial modulus relating axial stress (\sigma) and axial strain (\varepsilon):
    [ E = \frac{\sigma}{\varepsilon} ]


Principal Stresses and Strains

  • Stress tensor (\sigma) diagonalized to principal stresses: [ \sigma = \begin{bmatrix} \sigma_1 & 0 & 0 \ 0 & \sigma_2 & 0 \ 0 & 0 & \sigma_3 \end{bmatrix} ]

  • Strain tensor (\varepsilon) diagonalized to principal strains: [ \varepsilon = \begin{bmatrix} \varepsilon_1 & 0 & 0 \ 0 & \varepsilon_2 & 0 \ 0 & 0 & \varepsilon_3 \end{bmatrix} ]


Visualization (Mermaid.js)

graph LR
    O[Origin: Unit Sphere] --> SE[Strain Ellipsoid]
    O --> ST[Stress Ellipsoid]
    SE -->|Axes = Principal Strains| ε1[ε1], ε2[ε2], ε3[ε3]
    ST -->|Axes = Principal Stresses| σ1[σ1], σ2[σ2], σ3[σ3]

Summary

  • Use **strain ell
12Miscellaneous Terms

IS 11358 (1987) is primarily a glossary of terms and symbols related to rock mechanics, not a design or calculation code. It defines and standardizes terminology used across rock mechanics.

Key Points:

  • No formulas or tables are directly provided in IS 11358.
  • It serves as a reference for consistent use of terms in related IS codes.
  • Terms cover rock properties, stresses, discontinuities, and mechanical behavior.

Common Miscellaneous Terms in Rock Mechanics (examples):

TermDefinition
Uniaxial Compressive Strength (UCS)Maximum axial compressive stress rock can withstand
Modulus of Elasticity (E)Ratio of stress to strain in elastic deformation
Poisson’s Ratio (ν)Lateral strain to axial strain ratio
DiscontinuityAny plane or surface of weakness in rock mass

Usage:

Refer to IS 11358 for standard terminology when reading or preparing documentation and design based on other rock mechanics standards like IS 6925, IS 11282, etc.

flowchart LR
A[Rock Mass] --> B[Properties]
B --> C[Strength]
B --> D[Elasticity]
B --> E[Discontinuities]

For detailed formulas or tables, consult design codes or specialized rock mechanics standards.

Popular Questions About IS 11358

?What are the key rock properties defined in IS 11358?

IS 11358 defines key rock properties essential for rock mechanics and geotechnical descriptions. The Basic Geotechnical Description (BGD) includes five main parameters:

  • Rock Name (Geological Description): Identifies the rock type.
  • Layer Thickness (L): Thickness of the rock layer.
  • Fracture Intercept (F): Spacing or frequency of fractures.
  • Uniaxial Compressive Strength (S): Measure of rock strength under compression.
  • Angle of Friction of Fractures (A): Shear resistance angle along fractures.

Example notation:
Quartz - L2, F4, S3, A2
where L, F, S, A represent the respective parameters.

These parameters help characterize rock mass behavior for engineering design and analysis.

?How does this standard define and classify rock deformation?

IS 11358 defines and classifies rock deformation primarily through the classification of rock mass formations based on their structural features and seam characteristics:

  • Massive: Solid, dense rock mass with practically no seams; minimal deformation.
  • Sheets: Rock mass with layers/beds 1 to 3 m thick, thin horizontal seams.
  • Laminated: Thin layers (30 to 100 cm) with horizontal seams and little/no gouge.
  • Seamy: Many open seams both horizontally and vertically, indicating moderate deformation.
  • Blocky: Wide open seams in all directions, filled with gouge; rock is shattered or fissured, showing significant deformation.

This classification reflects the degree and nature of rock deformation, from intact (massive) to highly fractured (blocky).

Summary Table:

Rock TypeLayer ThicknessSeam ConditionDeformation Level
MassiveNone or negligiblePractically no seamsMinimal
Sheets1 to 3 mThin horizontal seamsLow
Laminated30 to 100 cmHorizontal seams, little/no gougeModerate
SeamyVariableMany open seams (H & V)Moderate to High
BlockyVariableWide open seams, gouge-filledHigh (shattered/fissured)

This classification aids in assessing rock stability and deformation behavior in engineering designs.

?What terms related to blasting and excavation are included?

IS 11358 Terms Related to Blasting and Excavation:

  • Bench Blasting (2.28): Excavation in steps or benches; blast holes drilled parallel to the free face in quarries/open pits.

  • Smooth Blasting (2.293): Minimizes rock damage by using closely spaced holes and light charges to reduce vibrations.

  • Controlled Blasting (2.67): Techniques (e.g., smooth blasting, presplitting) aimed at preserving rock integrity during blasting.

  • Blastability (2.31): An index measuring rock formation's resistance to blasting.


Summary Table

TermDescription
Bench BlastingStepwise excavation with parallel blast holes
Smooth BlastingLight charges, closely spaced holes to reduce damage
Controlled BlastingBlasting preserving rock integrity
BlastabilityRock resistance index to blasting

These terms guide safe, efficient excavation and rock breakage per IS 11358.

?How does IS 11358 address rock mass behavior under stress?

IS 11358 addresses rock mass behavior under stress primarily through defining key terms related to rock mechanics:

  • Shear Strength of a Rock Mass (Clause 2.278):
    The maximum resistance offered by a rock mass (including joints) to shearing stresses. This reflects how the rock mass will behave under shear loading conditions.

  • Stress Reduction Factor (SRF) (Clause 2.313):
    SRF quantifies the effect of stress changes due to excavation, considering:

    • Loosening pressure in shear zones or clay-bearing rocks
    • Ratio of uniaxial compressive strength (qc) to major principal stress (σ1) in competent rock
    • Squeezing or swelling pressures in weak rock masses

SRF acts as a comprehensive parameter representing the total stress state and its influence on rock mass stability.


Summary Table

ParameterDefinitionSignificance
Shear StrengthMax resistance to shear stressesStability against sliding/failure
Stress Reduction Factor (SRF)Measures stress changes due to excavationAccounts for loosening, squeezing, swelling pressures
Loading diagram...

This framework aids engineers in assessing rock mass behavior under various stress conditions per IS 11358.

?What symbols are standardized for stress and strain in rock mechanics?

According to IS 11358 (1987), which standardizes terms and symbols in rock mechanics:

Standardized Symbols for Stress and Strain

  • Stress (σ):

    • Symbol: σ
    • Unit: Pascal (Pa) or Megapascal (MPa)
    • Represents internal forces per unit area within rock.
  • Strain (ε):

    • Symbol: ε
    • Dimensionless (ratio)
    • Represents deformation per unit length (change in length/original length).

Additional Notes:

  • Stress components may be denoted as σ₁, σ₂, σ₃ for principal stresses.
  • Strain components may be denoted as ε₁, ε₂, ε₃ for principal strains.
  • Shear stress and strain use τ and γ respectively.
Loading diagram...

This standardization ensures uniform communication in rock mechanics analysis and design.

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