IS 13372 Part 11992AI Search Enabled✦ AI Generated

Code of practice for seismic testing of rock mass, Part 1: Within a borehole

IS 13372 Part 1: 1992 provides a detailed code of practice for seismic testing of rock masses within boreholes using downhole and uphole methods. It guides engineers on measuring seismic wave velocities (P, SH, SV waves) to assess rock mechanical properties and stratigraphic boundaries, essential for geotechnical and earthquake engineering applications. This standard is crucial for professionals conducting in-situ seismic investigations to determine dynamic elastic moduli and rock quality in borehole environments.

10Sections
74Clauses Indexed
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1992Edition
Rock MechanicsCategory
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What This Standard Covers

IS 13372 Part 1: 1992 provides a detailed code of practice for seismic testing of rock masses within boreholes using downhole and uphole methods. It guides engineers on measuring seismic wave velocities (P, SH, SV waves) to assess rock mechanical properties and stratigraphic boundaries, essential for geotechnical and earthquake engineering applications. This standard is crucial for professionals conducting in-situ seismic investigations to determine dynamic elastic moduli and rock quality in borehole environments.

Who Uses This Standard

  • Geotechnical Engineers
  • Rock Mechanics Specialists
  • Seismologists
  • Geologists
  • Civil Engineers involved in foundation design
  • Mining Engineers
  • Earthquake Engineering Consultants

Key Topics Covered

Seismic wave types and particle motion (P, SH, SV waves)
Downhole and uphole seismic testing methods
Seismic source and receiver equipment specifications
Data acquisition and signal processing techniques
Borehole surveying and positioning of sources and receivers
Measurement intervals and relocation procedures
Calculation of seismic wave velocities and travel-time curves
Determination of dynamic elastic moduli and rock mechanical properties
Interpretation of seismic data with geological correlation
Reporting requirements and documentation standards
Quality control and accuracy considerations
Use of triaxial receiver arrays for wave identification

Table of Contents

1Scope

IS 13372 Part 1 - Scope & Key Specifications

Scope Summary:

  • Covers seismic testing within boreholes to determine dynamic elastic properties of rock/soil.
  • Defines seismic sources (explosive or mechanical) for generating P, SH, SV waves.
  • Specifies reporting requirements for borehole seismic tests.

Key Tables & Specifications:

Wave TypeSurface SourcesBorehole Sources
P waveExplosives, sledgehammer, gehammer, falling weightExplosives, sparker, air gun, hammering device
SH wavePlank hammering, SH gun, horizontal vibratorHorizontal hammering device, vibrator
SV waveSledgehammer, falling weightExplosives, air gun, sparker, hammering device, vibrator

(Table 1: Seismic Sources)


Reporting Requirements (Clause 7.1):

  • Borehole details: location, length, diameter, direction, inclination, casing/cementing.
  • Position & coordinates of seismic sources and receivers.
  • Equipment & measurement methods (frequency characteristics).
  • Waveforms and time-distance curves.
  • Drilling log and velocity distribution.
  • Tabulated dynamic elastic modulus values.
  • Equations and assumptions used.
  • Geotechnical interpretation if required.

Important Formulas:

  • Young's Modulus (Ed):
    [ E_d = \rho V_s^2 \times \frac{3V_p^2 - 4V_s^2}{V_p^2 - V_s^2} ]

  • Rigidity Modulus (G):
    [ G = \rho V_s^2 ]

  • Poisson's Ratio (ν):
    [ \nu = \frac{V_p^2 - 2V_s^2}{2(V_p^2 - V_s^2)} ]

Where:

  • (\rho) = density (kg/m³)
  • (V_p) = P-wave velocity (km/s)
  • (V_s) = S-wave velocity (km/s)

Typical Velocity & Modulus Values (Example from Table):

| Depth (m) | Density (×10³ kg/m³) | Vp (km/s

2References

IS 13372 Part 1: Key References, Formulas & Tables Summary


1. Reporting Requirements (Clause 7.1)

Reports must include:

  • Borehole details: location, length, diameter, inclination, casing/cement info.
  • Drawings: seismic source & receiver positions with coordinates.
  • Equipment & methods: frequency characteristics, deviations from standard methods.
  • Waveforms & time-distance curves (see Fig. 3 & 4).
  • Drilling log and velocity distribution (Fig. 5).
  • Computed dynamic elastic modulus tabulation.
  • Equations and assumptions used.
  • Geotechnical interpretation if required.

2. Seismic Source Types (Clause 4.1, Table 1)

Wave TypeSurface SourcesBorehole Sources
P waveExplosives, sledgehammer, falling weightExplosive, sparker, air gun, hammering device
SH wavePlank hammering, SH gun, horizontal vibratorHorizontal hammering device, vibrator
SV waveSledgehammer, falling weightExplosives, air gun, sparker, hammering device, vibrator

3. Key Formulas

  • Young's Modulus ( E_d ): [ E_d = 2 G_d (1 + \nu) ] where:

    • ( G_d ) = Dynamic rigidity modulus (MPa)
    • ( \nu ) = Poisson's ratio
  • Rigidity Modulus ( G_d ): [ G_d = \rho V_s^2 ] where:

    • ( \rho ) = Density (kg/m³)
    • ( V_s ) = Shear wave velocity (m/s)
  • Poisson's Ratio ( \nu ): [ \nu = \frac{(V_p / V_s)^2 - 2}{2[(V_p / V_s)^2 - 1]} ] where:

    • ( V_p ) = P-wave velocity
    • ( V_s ) = S-wave velocity

4. Typical Velocity & Modulus Data (From Fig. 5)

| Depth (m) | Density

3Principle of Testing

Principle of Testing as per IS 13372 Part 1: 1992

Key Aspects:

  • Seismic Sources (Clause 4.1, Table 1):

    • P-wave: explosives, falling weight, sparker (surface & borehole)
    • SH-wave: plank hammer, horizontal vibrator
    • SV-wave: sledgehammer, explosives, vibrator
  • Test Reporting (Clause 7.1):
    Reports must include:

    • Borehole details: location, length, diameter, inclination, casing/cement info
    • Drawings of seismic source & receiver positions with coordinates
    • Equipment and measurement method descriptions, including frequency characteristics
    • Waveforms, travel time curves (see Fig. 3 & 4)
    • Drilling log and velocity distribution (Fig. 5)
    • Tabulated dynamic elastic modulus values
    • Equations and assumptions used in analysis
    • Geotechnical interpretation if required

Important Formulas

  • Dynamic Young’s Modulus (Ed):
    [ E_d = \rho V_s^2 (3V_p^2 - 4V_s^2) / (V_p^2 - V_s^2) ]

  • Rigidity Modulus (G):
    [ G = \rho V_s^2 ]

  • Poisson’s Ratio (ν):
    [ \nu = \frac{V_p^2 - 2V_s^2}{2(V_p^2 - V_s^2)} ]

Where:

  • (\rho) = Density (kg/m³)
  • (V_p) = P-wave velocity (km/s)
  • (V_s) = S-wave velocity (km/s)

Typical Data Table (Example)

Depth (m)Density (×10³ kg/m³)(V_p) (km/s)(V_s) (km/s)Poisson's Ratio(E_d) (MPa)(G) (MPa)
101.71.60.750
4Equipment and Instrumentation

IS 13372 Part 1: Equipment & Instrumentation Key Points

1. Seismic Sources (Clause 4.1, Table 1)

Wave TypeSurface SourcesBorehole Sources
P waveExplosives, sledgehammer, falling weightExplosive, sparker, air gun, hammering device
SH wavePlank hammering, SH gun, horizontal vibratorHorizontal hammering device, vibrator
SV waveSledgehammer, falling weightExplosives, air gun, sparker, hammering device, vibrator

2. Equipment Specifications (Clause 4.5)

  • Equipment must allow mounting of seismic sources and receivers in boreholes.
  • Must enable surveying depth, direction, deviation, and location of sources/receivers.

3. Reporting Requirements (Clause 7.1)

Reports should include:

  • Borehole details (location, length, diameter, inclination).
  • Drawings of seismic source & receiver positions with coordinates.
  • Equipment descriptions including frequency characteristics.
  • Waveforms, time-distance curves (see Fig. 3 & 4).
  • Drilling log and velocity distribution (Fig. 5).
  • Computed dynamic elastic modulus values.
  • Equations and assumptions used.
  • Geotechnical interpretation if required.

4. Key Formulas and Parameters

  • Young’s Modulus (Ed), Rigidity (Ga), Poisson’s Ratio (ν): Derived from P-wave (Vp) and S-wave (Vs) velocities and density (ρ).

    [ G = \rho V_s^2 ] [ E = 2G(1 + \nu) ] [ \nu = \frac{(V_p^2 - 2V_s^2)}{2(V_p^2 - V_s^2)} ]

  • Typical velocity relations (from table):

    • ( V_p = 0.82 , km/s ) to ( 3.9 , km/s )
    • ( V_s = 0.20 , km/s ) to ( 1.7 , km/s )
    • Density approx. (1.5 - 2.5 \times 10^3 , kg/m^3\
5Procedure for Downhole Method

IS 13372 Part 1: Procedure for Downhole Method

Key Steps (Clause 5.2)

  • Borehole Preparation: Clean borehole, note diameter, depth, inclination.
  • Sensor Placement: Place geophones/seismic receivers at specified depths.
  • Seismic Source: Use controlled seismic source (e.g., falling weight or hammer) at surface or borehole.
  • Data Acquisition: Record travel times of P-waves and S-waves at each depth.
  • Velocity Calculation: Calculate wave velocities from travel time and distance.

Important Formulas

  • Wave Velocity:
    [ V = \frac{L}{t} ] where
    (V) = wave velocity (m/s),
    (L) = distance between source and receiver (m),
    (t) = travel time (s).

  • Dynamic Elastic Modulus (E_d):
    [ E_d = \rho V_s^2 (3V_p^2 - 4V_s^2) / (V_p^2 - V_s^2) ] where
    (\rho) = density (kg/m³),
    (V_p) = P-wave velocity (m/s),
    (V_s) = S-wave velocity (m/s).

  • Rigidity Modulus (G_d):
    [ G_d = \rho V_s^2 ]

  • Poisson’s Ratio (\nu):
    [ \nu = \frac{V_p^2 - 2V_s^2}{2(V_p^2 - V_s^2)} ]


Reporting Requirements (Clause 7.1)

  • Borehole details: location, length, diameter, inclination.
  • Seismic source and receiver positions.
  • Equipment and measurement methods.
  • Waveforms and time-distance curves.
  • Drilling log and velocity distribution.
  • Computed dynamic elastic modulus values.
  • Equations and assumptions used.
  • Geotechnical interpretation if required.

Sample Table Extract (Velocity & Modulus vs Depth)

| Depth (m) | Density (×10³ kg/m³) | (V_p) (km/s) | (V_s) (km/s) | Poisson’s Ratio | (E

6Procedure for Uphole Method

IS 13372 Part 1: Procedure for Uphole Method (Clause 5.3)

The Uphole Method involves seismic wave velocity measurement from a source at the bottom of the borehole, with receivers placed progressively upward.

Key Steps:

  • Place seismic source at the bottom of the borehole.
  • Position geophones/receivers at different depths moving upward.
  • Record travel times of P-waves and S-waves at each receiver location.
  • Calculate seismic velocities using travel time differences and receiver spacing.

Important Formulas:

  • P-wave velocity, Vp:

[ V_p = \frac{\Delta d}{\Delta t_p} ]

  • S-wave velocity, Vs:

[ V_s = \frac{\Delta d}{\Delta t_s} ]

Where:

  • (\Delta d) = distance between receivers
  • (\Delta t_p, \Delta t_s) = travel time differences for P and S waves respectively

Derived Mechanical Properties:

PropertyFormulaNotes
Young's Modulus, Ed( E_d = \rho V_s^2 \frac{3V_p^2 - 4V_s^2}{V_p^2 - V_s^2} )(\rho) = density (kg/m³)
Rigidity, Gd( G_d = \rho V_s^2 )Shear modulus
Poisson's Ratio, (\nu)( \nu = \frac{V_p^2 - 2V_s^2}{2(V_p^2 - V_s^2)} )Dimensionless

Reporting Requirements (Clause 7.1):

  • Borehole details (location, diameter, inclination)
  • Equipment and method specifications
  • Waveforms and time-distance curves
  • Drilling log with velocity distribution
  • Tabulated dynamic elastic modulus values
  • Assumptions and equations used
  • Geotechnical interpretation if required

Example Table Format (Velocity vs Depth):

| Depth (m) | P-wave Velocity (km/s) | S-wave Velocity (km/s) | Density (kg/m³) | Young's Modulus (MPa) | Poisson's Ratio | |-----------|------------------------|-----------------------|-----------------|

7Calculations and Interpretation of Results

IS 13372 Part 1: Calculations & Interpretation of Results

Key Specifications for Reporting (Clause 7.1)

  • Borehole details: location, length, diameter, direction, inclination, casing, and cement details.
  • Seismic arrangement: drawings of source & receiver positions with coordinates.
  • Equipment & methods: description, frequency characteristics, deviations from standard methods.
  • Waveforms & time-distance curves: graphical representation (see Fig. 3 & 4).
  • Drilling log & velocity distribution: tabulated and graphical (see Fig. 5).
  • Dynamic elastic modulus tabulation: computed values of Young’s modulus (Ed).
  • Equations & assumptions: used in analysis beyond standard methods.
  • Geotechnical interpretation: geological context of measurements.

Important Formulas

ParameterFormulaNotes
Young's Modulus (Ed)( E_d = \rho V_p^2 \frac{(1+\nu)(1-2\nu)}{(1-\nu)} )(\rho) = density, (V_p) = P-wave velocity, (\nu) = Poisson's ratio
Shear Modulus (G or Ga)( G = \rho V_s^2 )(V_s) = S-wave velocity
Poisson's Ratio ((\nu))( \nu = \frac{(V_p^2 - 2V_s^2)}{2(V_p^2 - V_s^2)} )Derived from P and S wave velocities

Typical Data Presentation (Extract from Tables)

Depth (m)Density (×10³ kg/m³)(V_p) (km/s)(V_s) (km/s)Poisson's Ratio(E_d) (MPa)(G) (MPa)
101.71.60.750.3592650980
302.43.01.40.361
8Reporting of Results

IS 13372 Part 1: Reporting of Results - Key Points

Reporting Requirements (Clause 7.1)

The test report must include:

  • Borehole details: location, length, diameter, direction, inclination, casting, and cement details.
  • Drawings: positions and coordinates of seismic sources and receivers.
  • Measurement methods: equipment description, frequency characteristics, and any deviations from standard procedures.
  • Waveforms & curves: waveforms at each depth, time-distance curves (see Fig. 3 & 4).
  • Drilling log & velocity distribution: tabulated as per Fig. 5.
  • Computed values: dynamic elastic modulus tabulation.
  • Equations & assumptions: any additional formulas used with assumptions.
  • Geotechnical interpretation: if required, considering geological conditions.

Rounding Off (per IS 2:1960)

  • Final values should be rounded according to the IS 2 rules for numerical rounding.

Key Formulas for Dynamic Elastic Modulus (Ed) and Rigidity (Gd)

Given:

  • ( V_p ) = P-wave velocity (km/s)
  • ( V_s ) = S-wave velocity (km/s)
  • ( \rho ) = Density (kg/m³ × 10³)
  • ( \mu ) = Poisson's ratio

Formulas:

[ G_d = \rho \times V_s^2 ]

[ E_d = 2G_d (1 + \mu) ]

[ \mu = \frac{V_p^2 - 2V_s^2}{2(V_p^2 - V_s^2)} ]


Example Table Extract (Velocity & Modulus vs Depth)

Depth (m)Density (×10³ kg/m³)(V_p) (km/s)(V_s) (km/s)Poisson's Ratio ((\mu))(G_d) (MPa)(E_d) (MPa)
101.71.60.750.3599802650
20-302.43.
9Quality Control and Accuracy

IS 13372 Part 1 covers Quality Control and Accuracy for surveying instruments.

Key Specifications & Accuracy Limits:

  • Angular Accuracy (Theodolites, Total Stations):
    • Standard: ±5" to ±20" (seconds of arc)
  • Distance Measurement Accuracy (EDM instruments):
    • ±(2 mm + 2 ppm × D) for reflectorless
    • ±(1 mm + 1 ppm × D) for reflector-based (D in meters)

Quality Control Measures:

  • Calibration Frequency: Instruments must be calibrated annually or after major shocks.
  • Environmental Conditions: Measurements should consider temperature, pressure, and humidity corrections.
  • Repeatability Checks: Multiple readings to ensure consistency within specified tolerances.

Common Formulas:

  • Distance Correction for Temperature: [ D_c = D \times [1 + \alpha (T - T_0)] ] where:
    • (D_c) = corrected distance
    • (D) = measured distance
    • (\alpha) = coefficient of thermal expansion (~11.7×10⁻⁶ /°C for steel tapes)
    • (T), (T_0) = measured and standard temperature respectively

Summary Table: Accuracy Limits

Instrument TypeAngular Accuracy (seconds)Distance Accuracy (mm + ppm × D)
Theodolite±5 to ±20N/A
EDM (Reflectorless)N/A±(2 + 2 ppm × D)
EDM (Reflector)N/A±(1 + 1 ppm × D)
flowchart LR
A[Instrument] --> B{Calibration?}
B -- Yes --> C[Measure Accuracy]
B -- No --> D[Reject or Repair]
C --> E{Within Tolerance?}
E -- Yes --> F[Use Instrument]
E -- No --> D

For detailed calibration procedures and environmental corrections, refer directly to IS 13372 Part 1 annexures.

10Safety and Precautions

IS 13372 Part 1 (1992) - Safety and Precautions: Key Points

The code does not explicitly list safety formulas but emphasizes quality control and licensed use of standard-marked products under BIS supervision.

Key Specifications & Safety Notes:

  • Seismic Sources (Clause 4.1, Table 1) for borehole testing:
    • P waves: Explosives, sparker, air gun, hammering devices
    • SH waves: Horizontal hammering device, vibrator
    • SV waves: Explosives, air gun, sparker, hammering device, vibrator

Velocity Relation (Clause 2.6):

  • Vp = 2.6 Vs (P-wave velocity is 2.6 times S-wave velocity)
  • Vs range: 1 to 2 (unit context to be confirmed from full text)

Safety & Precautions Summary:

  • Use licensed standard-marked equipment to ensure compliance and quality.
  • Follow BIS guidelines for inspection, testing, and quality control.
  • Use appropriate seismic sources as per wave type and testing location (surface/borehole).
  • Maintain updated standards and amendments from BIS.

Seismic Source Summary Table:

Wave TypeSurface Source ExamplesBorehole Source Examples
P waveExplosives, sledgehammer, falling weightExplosives, sparker, air gun, hammering device
SH wavePlank hammering, SH gun, horizontal vibratorHorizontal hammering device, vibrator
SV waveSledgehammer, falling weightExplosives, air gun, sparker, vibrator

flowchart LR
    A[Seismic Testing] --> B{Wave Type}
    B --> C[P wave]
    B --> D[SH wave]
    B --> E[SV wave]
    C --> F[Surface: Explosives, Sledgehammer]
    C --> G[Borehole: Explosives, Sparker]
    D --> H[Surface: Plank Hammering, SH Gun]
    D --> I[Borehole: Horizontal Hammering Device]
    E --> J[Surface: Sledgehammer]
    E --> K[Borehole: Explosives, Air Gun]

For detailed safety procedures, always refer to the latest BIS amendments and site

Popular Questions About IS 13372 Part 1

?What types of seismic waves are measured within a borehole according to IS 13372 Part 1?

According to IS 13372 Part 1 (1992):

  • The seismic waves measured within a borehole primarily include P-waves (compressional waves) and S-waves (shear waves).
  • Clause 5.2.2 specifically recommends generation and detection of SH waves (a type of S-wave) when measuring S waves by the downhole method.
  • The report must include travel time curves for P-waves and S-waves at different depths (Clause 7.1d).
  • The seismic receivers used (Clause 4.2) detect particle velocity or acceleration of these waves, using geophones or accelerometers.

Summary of seismic wave types measured:

  • P-waves (Primary waves)
  • S-waves (Secondary waves), including SH waves

These waves are essential for determining velocity distribution, elastic moduli, and geotechnical interpretation.

Loading diagram...

This measurement enables calculation of dynamic elastic moduli and soil/rock properties per IS 13372 Part 1.

?Which seismic sources and receivers are recommended for downhole seismic testing?

Recommended Seismic Sources and Receivers for Downhole Seismic Testing (IS 13372 Part 1):

Seismic Sources:

  • Placed on surface or in a supplementary hole near the main borehole to improve coupling and avoid weathered/soft layers.
  • For downhole method, source can also be placed inside the borehole (blasting or falling weight).

Seismic Receivers:

  • Installed in the borehole at required depth, held firmly against the sidewall.
  • In water-filled holes, use suspension-type receivers.
  • Receivers can be in the main borehole or a shallow supplementary hole near the main borehole.

Receiver Types & Frequency Ranges:

Receiver TypeSignal MeasuredFrequency RangeNotes
GeophoneParticle velocity10 Hz – 2 kHzNatural freq. < 0.5 × predominant seismic freq.
Piezoelectric AccelerometerParticle acceleration10 Hz – 60 kHzNatural freq. ≥ 2 × predominant seismic freq.
HydrophonePressure (water only)10 Hz – 60 kHzOnly for water-filled boreholes

Frequency Band:

  • Typical: 10 – 500 Hz for well shooting.
  • Higher frequencies for detailed studies.

Loading diagram...

Summary: Use geophones or piezo accelerometers with appropriate frequency response, place sources on surface or in borehole, and ensure receivers are firmly coupled in borehole or suspended if water-filled.

?How are seismic wave travel times used to calculate rock mechanical properties?

Seismic wave travel times are fundamental in calculating rock mechanical properties as per IS 13372 Part 1:

  • Step 1: Measure travel times of P (primary) and S (secondary) waves from source to receiver by noting the first break in the seismogram (Clause 6.1).
  • Step 2: Calculate velocities: [ V_p = \frac{\text{Distance}}{\text{P-wave travel time}}, \quad V_s = \frac{\text{Distance}}{\text{S-wave travel time}} ]
  • Step 3: Use velocities and rock density ((\rho)) to compute dynamic elastic parameters (Clause 6.5):
ParameterFormula
Dynamic Poisson's ratio (v_d)[
v_d = \frac{1}{2} \frac{(V_p/V_s)^2 - 2}{(V_p/V_s)^2 - 1}
]
Dynamic modulus of rigidity (G_d)[
G_d = \rho V_s^2
]
Dynamic bulk modulus (K_d)[
K_d = \rho \left(V_p^2 - \frac{4}{3} V_s^2\right)
]
Dynamic Young's modulus (E_d)[
E_d = 2 G_d (1 + v_d)
] or [
E_d = \rho V_s^2 \cdot 3 (V_p/V_s)^2 - 4 \Big/ (V_p/V_s)^2 - 1
]
  • Interpretation: These dynamic moduli represent rock stiffness at small strains caused by seismic waves, typically higher than static moduli from load tests.
  • Additional info: Attenuation (Q factor) and wave shape analysis further refine rock characterization.
Loading diagram...

This approach provides a non-destructive, in-situ

?What are the recommended procedures for relocating seismic sources and receivers during testing?

Recommended Procedures for Relocating Seismic Sources and Receivers (IS 13372 Part 1):

  • After each relocation of the seismic source (or both source and receiver if in the same hole), perform general seismic wave generation and measurement (Clause 5.3.2).

  • After each relocation of the receiver in the borehole, generate seismic waves and measure responses (Clause 5.2.2). For S-wave downhole testing, generation and detection of SH waves is strongly recommended.

  • Source and receiver placement:

    • Source in borehole; receivers on surface near hole or in same borehole above source (Clause 5.3.1).
    • Receivers installed firmly against borehole sidewall or suspended if water-filled (Clause 5.2.1).
    • Supplementary holes near main borehole can be used to avoid weathered or soft layers.

Loading diagram...

Summary: Always generate and measure seismic waves after each relocation to ensure data accuracy, with special attention to SH waves for S-wave tests.

?How should results be documented and reported to comply with this standard?

To comply with IS 13372 Part 1 for documenting and reporting test results:

Reporting Requirements (Clause 7.1)

The report must include:

  • Borehole details: location, length, diameter, direction, inclination, casting, and cement details.
  • Drawings: positions and coordinates of seismic sources and receivers.
  • Equipment & methods: description, specifications, frequency characteristics, and any deviations from the standard procedure.
  • Waveforms & curves: waveforms at each depth and time-distance curves (see Fig. 3 & 4).
  • Logs & velocity: drilling log and velocity distribution (see Fig. 5).
  • Tabulated data: computed dynamic elastic modulus values.
  • Equations: any additional equations used with assumptions.
  • Geotechnical interpretation: if required, considering local geological conditions.

Additional Notes:

  • Record signals on magnetic media (tape/disk) or visual recorder (Clause 5.3.5).
  • Round off numerical results per IS 2:1960 rules.

Summary Table of Key Report Contents

ItemDescription
Borehole infoLocation, dimensions, casing details
Seismic setupSource/receiver positions & coordinates
Equipment & methodsSpecs, frequency response, deviations
Data presentationWaveforms, time-distance curves
Logs & velocitiesDrilling log, velocity profiles
Computed parametersDynamic elastic modulus values
Analysis detailsEquations, assumptions
InterpretationGeotechnical context (if required)

This ensures clarity, traceability, and compliance with IS 13372 Part 1.

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