IS 11315 PART 61987AI Search Enabled✦ AI Generated

Method for the quantitative description of discontinuities in rock masses, Part 6: Aperture
1987 Edition

The 1987 edition of IS 11315 Part 6 establishes a uniform procedure for quantitatively describing the aperture of rock mass discontinuities. It defines aperture as the orthogonal gap between adjoining rock surfaces within an open discontinuity. This standard serves as a vital resource for professionals engaged in rock mass evaluation, offering measurement protocols, classification schemes, and reporting guidelines to aid in geotechnical and rock engineering applications.

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1987Edition
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What This Standard Covers

The 1987 edition of IS 11315 Part 6 establishes a uniform procedure for quantitatively describing the aperture of rock mass discontinuities. It defines aperture as the orthogonal gap between adjoining rock surfaces within an open discontinuity. This standard serves as a vital resource for professionals engaged in rock mass evaluation, offering measurement protocols, classification schemes, and reporting guidelines to aid in geotechnical and rock engineering applications.

Who Uses This Standard

  • Geotechnical engineering professionals
  • Specialists in rock mechanics
  • Geological experts
  • Mining industry engineers
  • Civil engineers focused on rock foundations
  • Engineers working on tunnel and slope stability
  • Hydrogeologists

Key Topics Covered

Concept and importance of aperture in rock discontinuities
Techniques for gauging apertures including feeler gauges and measuring tapes
Classification system ranging from closed to cavernous aperture widths
Impact of aperture on mechanical properties and fluid flow in rock masses
Field survey methods and preparation of rock surfaces for aperture measurement
Utilization of borehole periscopes and core sampling for aperture evaluation
Difficulties in measuring disturbed versus intact apertures
Standards for documenting and presenting aperture measurements, including photographic records
Correlation between aperture size and shear strength of rock joints
Applying aperture measurements in rock mass characterization and design
Limitations of visual aperture estimation and the role of in situ permeability testing

Table of Contents

0Overview and Introduction

Introduction to IS 11315 Part 6: Aperture in Rock Discontinuities

Scope Summary:

  • Provides a method for quantitatively describing the aperture in rock mass discontinuities.
  • Defines aperture as the perpendicular spacing between adjoining rock walls, which may be air or water filled.

Aperture Classification (Clause 5.1, Table 1)

Aperture WidthDescriptionNotes
< 0.25 mmTight'Closed' discontinuity
0.25 - 0.5 mmPartially open
0.5 - 2.5 mmOpen
2.5 - 10 mmModerately wide'Gapped' discontinuity
> 10 mmWide
1 - 10 cmVery wide
10 - 100 cmExtremely wide'Open' discontinuity
> 1 mCavernous

SI Units and Derived Units (Clause 5.4)

QuantityUnitSymbolDefinition
Lengthmetrem
ForcenewtonN1 N = 1 kg·m/s²
Pressure, stresspascalPa1 Pa = 1 N/m²
EnergyjouleJ1 J = 1 N·m
PowerwattW1 W = 1 J/s
FrequencyhertzHz1 Hz = 1 cycle/s

Important Remarks

  • Apertures classified as extremely wide (10–100 cm) and cavernous (>1 m) require photographic documentation.
  • Classification assists in predicting rock mass behavior and supports engineering design.
  • Measurement results should be rounded as per IS 2-1960.
1Scope and Fundamental Definitions

IS 11315 Part 6: Defining the Scope and Aperture Terminology

Scope:

  • Establishes aperture as the perpendicular distance between adjacent rock walls within a discontinuity, which may contain air or water.
  • Provides a systematic approach to describe discontinuities influencing rock mass mechanical properties.
  • Forms part of a comprehensive system addressing various discontinuity parameters such as orientation, spacing, roughness, and filling.

Aperture Categories (Table 1)

Aperture RangeDescriptionRemarks
< 0.25 mmTightClassified as 'Closed'
0.25 - 0.5 mmPartly open
0.5 - 2.5 mmOpen
2.5 - 10 mmModerately wideTermed 'Gapped'
> 10 mmWide
1 - 10 cmVery wide
10 - 100 cmExtremely wideConsidered 'Open'
> 1 mCavernous

Relevant Units for Rock Mechanics

QuantityUnitSymbolDefinition
Lengthmetrem
ForcenewtonN1 N = 1 kg·m/s²
Pressure/StresspascalPa1 Pa = 1 N/m²

Notes on Data Presentation

  • Photographic records are recommended for very wide and cavernous apertures.
  • Final values must conform to rounding rules specified in IS 2-1960.
graph TD
    A[Rock Mass Discontinuity] --> B[Aperture Measurement]
    B --> C{Aperture Size}
    C -->|<0.25 mm| D[Tight (Closed)]
    C -->|0.25 - 0.5 mm| E[Partly Open]
    C -->|0.5 - 2.5 mm| F[Open]
    C -->|2.5 - 10 mm| G[Moderately Wide]
    C -->|> 10 mm| H[Wide]
    C -->|1 - 10 cm| I[Very Wide]
    C -->|10 - 100 cm| J[Extremely Wide]
    C -->|> 1 m| K[Cavernous]
2Terminology and Measurement Units

Terminology and Definitions in IS 11315 Part 6

  • Aperture: The orthogonal separation between adjacent rock surfaces forming an open discontinuity, potentially filled with air or water.
  • Discontinuity: A mechanical break or weakness such as joints, faults, or shear zones characterized by limited tensile strength.

Aperture Size Classification (Clause 5.1, Table 1)

Aperture WidthDescriptionNotes
< 0.25 mmTightDenoted as 'Closed'
0.25 - 0.5 mmPartly open
0.5 - 2.5 mmOpen
2.5 - 10 mmModerately wideTermed 'Gapped'
> 10 mmWide
1 - 10 cmVery wide
10 - 100 cmExtremely wideConsidered 'Open'
> 1 mCavernous

SI Units and Related Units (Clause 5.4)

QuantityUnitSymbolDefinition
Lengthmetrem
ForcenewtonN1 N = 1 kg·m/s²
Pressure/StresspascalPa1 Pa = 1 N/m²
EnergyjouleJ1 J = 1 N·m
PowerwattW1 W = 1 J/s

Additional Notes

  • Apply rounding as per IS 2-1960.
  • Include photographic evidence for apertures exceeding 10 cm.
3Field Measurement Techniques

Procedures for Field Measurement of Aperture (IS 11315 Part 6)

  • Instruments:

    • For small apertures (<10 mm): feeler gauges are preferred.
    • For larger apertures (>10 mm): steel rulers or tapes calibrated in millimeters.
  • Methodology:

    • Document apertures of all discontinuities intersecting the measurement line.
    • For prominent discontinuities, note aperture variation along their trace.
  • Special Techniques:

    • Borehole periscopes equipped with calibrated scales allow aperture measurement up to depths of approximately 30 meters.
    • Integral sampling with reinforced core extraction may be employed for specific scenarios.
  • Considerations:

    • Surface aperture measurements may overestimate actual rock mass apertures due to weathering or excavation effects.
    • Aperture alone is insufficient to predict water flow; permeability tests are recommended.
    • Aperture dimensions can vary significantly in sheared or displaced joints.

Aperture Classification (Table 1)

Aperture WidthDescriptionNotes
< 0.25 mmTight'Closed' features
0.25 - 0.5 mmPartly open
0.5 - 2.5 mmOpen
2.5 - 10 mmModerately wide'Gapped' features
> 10 mmWide
1 - 10 cmVery wide
10 - 100 cmExtremely wide'Open' features
> 1 mCavernous

Units (SI Units)

QuantityUnitSymbolDefinition
Lengthmetrem
ForcenewtonN1 N = 1 kg·m/s²
PressurepascalPa1 Pa = 1 N/m²

Diagram Overview

graph TD
    A[Perform Aperture Measurement] --> B{Aperture Size}
    B -->|<10 mm| C[Use Feeler Gauges]
    B -->|≥10 mm| D[Use Steel Rule or Tape]
    E[Borehole] --> F[Periscope (≤30 m depth)]
    E --> G[Camera and TV Inspection]
    E --> H[Pressure Packers]
    I[Special Cases] --> J[Integral Sampling Method]
4Reporting and Documentation of Aperture Data

Guidelines for Presenting Aperture Measurement Results (IS 11315 Part 6, Clause 5)

  • Aperture Classification (Table 1):
Aperture WidthDescriptionNotes
< 0.25 mmTight'Closed' features
0.25 - 0.5 mmPartly open
0.5 - 2.5 mmOpen
2.5 - 10 mmModerately wide'Gapped' features
> 10 mmWide
1 - 10 cmVery wide
10 - 100 cmExtremely wide'Open' features
> 1 mCavernous
  • Measurement Notes:

    • Use feeler gauges for fine apertures.
    • Employ millimeter-scaled rulers for larger gaps.
    • Surface weathering or excavation may distort aperture sizes.
    • Borehole periscopes are recommended for depths up to 30 meters.
    • Correct measurements if boreholes intersect discontinuities at angles other than 90°.
  • Photographic Documentation:

    • Include images for apertures classified as extremely wide and cavernous to support records.
  • Measurement Units:

    • Length in metres (m)
    • Force in newtons (N) where 1 N = 1 kg·m/s²
    • Pressure in pascals (Pa) where 1 Pa = 1 N/m²

Aperture Classification Flowchart

graph LR
    A[Tight < 0.25 mm] --> B[Partly Open 0.25 - 0.5 mm]
    B --> C[Open 0.5 - 2.5 mm]
    C --> D[Moderately Wide 2.5 - 10 mm]
    D --> E[Wide > 10 mm]
    E --> F[Very Wide 1 - 10 cm]
    F --> G[Extremely Wide 10 - 100 cm]
    G --> H[Cavernous > 1 m]
5Measurement Challenges and Accuracy Considerations

Limitations and Precautions in Aperture Measurement (IS 11315 Part 6)

  • Measurement Techniques:

    • Small apertures are estimated approximately using feeler gauges.
    • Larger apertures are measured with millimeter-graded rulers.
    • Borehole apertures are assessed via periscopes up to 30 meters depth, borehole cameras, TV inspection, or pressure-sensitive packers.
  • Challenges:

    • Surface apertures often appear larger than actual due to weathering or excavation disturbances.
    • Machine-drilled tunnels and boreholes yield more accurate, undisturbed aperture data.
    • Optical distortions limit periscope use beyond 30 meters.
    • Aperture size varies along discontinuities because of asperities and debris accumulation.
    • Aperture dimensions alone do not reliably predict water permeability since surface roughness and flow paths affect conductivity.
  • Accuracy Notes:

    • Correct aperture values for borehole angles if intersections with discontinuities are not perpendicular.
    • Integral sampling with reinforced core bars is advised for special cases.
    • Aperture measurements should be supplemented with in situ permeability testing for hydraulic assessments.

Aperture Size Classification (Table 1)

Aperture WidthDescriptionNotes
< 0.25 mmTight'Closed' features
0.25 - 0.5 mmPartly open
0.5 - 2.5 mmOpen
2.5 - 10 mmModerately wide'Gapped' features
> 10 mmWide
1 - 10 cmVery wide
10 - 100 cmExtremely wide'Open' features
> 1 mCavernous

SI Units Reference

QuantityUnitSymbolDefinition
Lengthmetrem
ForcenewtonN1 N = 1 kg·m/s²
Pressure/StresspascalPa1 Pa = 1 N/m²

Popular Questions About IS 11315 PART 6

?How does the standard define and categorize aperture in rock discontinuities?

According to IS 11315 Part 6, aperture is defined as the perpendicular gap between adjacent rock faces in an open discontinuity, which may be filled with air or water. The standard classifies apertures into sizes ranging from tight (<0.25 mm) to cavernous (>1 m), with intermediate categories such as partly open, open, moderately wide (gapped), wide, very wide, and extremely wide. This classification enables consistent field descriptions and supports engineering assessments.

?What tools and approaches are recommended for measuring aperture in the field?

The standard recommends using feeler gauges for measuring fine apertures less than 10 mm, and steel rulers or calibrated measuring tapes for larger apertures. For borehole measurements, optical periscopes (effective up to 30 meters depth), borehole cameras, TV inspection equipment, and pressure-sensitive packers are suggested. Additionally, integral sampling involving reinforced core extraction may be used for special cases. Orientation corrections should be applied for boreholes intersecting discontinuities obliquely.

?In what ways does aperture influence the mechanical and hydraulic behavior of rock masses?

Aperture size significantly affects rock mass mechanical properties and fluid flow. Large apertures, often arising from shear displacement or erosion, can reduce joint interlocking and shear strength, thereby decreasing overall rock mass stability. Hydraulically, wider apertures enhance permeability and fluid transmissivity within rock joints. However, visual aperture measurements alone are unreliable for assessing water conductivity; in situ permeability tests provide more accurate evaluations.

?What difficulties arise when measuring aperture on disturbed rock surfaces?

Measuring aperture on disturbed rock exposures is complicated by factors such as surface weathering and excavation practices, which often enlarge apparent apertures relative to in situ conditions. Visual and tape measurements on such surfaces tend to be unreliable. Rough or dirty surfaces may obscure discontinuities, though the use of white spray paint can improve visibility. Variability along discontinuities due to asperity contact and debris further complicates measurements. More dependable data are obtained from machine-drilled tunnels, boreholes, and borehole-based tools like periscopes and cameras, supplemented with permeability testing.

?What are the recommended procedures for recording and reporting aperture measurements as per IS 11315 Part 6?

The standard advises measuring fine apertures approximately with feeler gauges and larger apertures with millimeter-graded rulers. All discontinuities intersecting the survey line should have their apertures recorded, noting variations along the discontinuity trace where applicable. Borehole aperture measurements should be conducted with periscopes or cameras, correcting for borehole orientation if necessary. The integral sampling method is recommended for specific cases requiring core recovery. Results must be rounded according to IS 2-1960, and photographic documentation should accompany records of extremely wide and cavernous apertures to ensure completeness.

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