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.
Overview
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.
Audience
Contents
Structure
IS 13372 Part 1 - Scope & Key Specifications
| Wave Type | Surface Sources | Borehole Sources |
|---|---|---|
| P wave | Explosives, sledgehammer, gehammer, falling weight | Explosives, sparker, air gun, hammering device |
| SH wave | Plank hammering, SH gun, horizontal vibrator | Horizontal hammering device, vibrator |
| SV wave | Sledgehammer, falling weight | Explosives, air gun, sparker, hammering device, vibrator |
(Table 1: Seismic Sources)
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:
| Depth (m) | Density (×10³ kg/m³) | Vp (km/s
IS 13372 Part 1: Key References, Formulas & Tables Summary
Reports must include:
| Wave Type | Surface Sources | Borehole Sources |
|---|---|---|
| P wave | Explosives, sledgehammer, falling weight | Explosive, sparker, air gun, hammering device |
| SH wave | Plank hammering, SH gun, horizontal vibrator | Horizontal hammering device, vibrator |
| SV wave | Sledgehammer, falling weight | Explosives, air gun, sparker, hammering device, vibrator |
Young's Modulus ( E_d ): [ E_d = 2 G_d (1 + \nu) ] where:
Rigidity Modulus ( G_d ): [ G_d = \rho V_s^2 ] where:
Poisson's Ratio ( \nu ): [ \nu = \frac{(V_p / V_s)^2 - 2}{2[(V_p / V_s)^2 - 1]} ] where:
| Depth (m) | Density
Key Aspects:
Seismic Sources (Clause 4.1, Table 1):
Test Reporting (Clause 7.1):
Reports must include:
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:
| Depth (m) | Density (×10³ kg/m³) | (V_p) (km/s) | (V_s) (km/s) | Poisson's Ratio | (E_d) (MPa) | (G) (MPa) |
|---|---|---|---|---|---|---|
| 10 | 1.7 | 1.6 | 0.75 | 0 |
IS 13372 Part 1: Equipment & Instrumentation Key Points
| Wave Type | Surface Sources | Borehole Sources |
|---|---|---|
| P wave | Explosives, sledgehammer, falling weight | Explosive, sparker, air gun, hammering device |
| SH wave | Plank hammering, SH gun, horizontal vibrator | Horizontal hammering device, vibrator |
| SV wave | Sledgehammer, falling weight | Explosives, air gun, sparker, hammering device, vibrator |
Reports should include:
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):
IS 13372 Part 1: Procedure for Downhole Method
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)}
]
| Depth (m) | Density (×10³ kg/m³) | (V_p) (km/s) | (V_s) (km/s) | Poisson’s Ratio | (E
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.
[ V_p = \frac{\Delta d}{\Delta t_p} ]
[ V_s = \frac{\Delta d}{\Delta t_s} ]
Where:
| Property | Formula | Notes |
|---|---|---|
| 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 |
| Depth (m) | P-wave Velocity (km/s) | S-wave Velocity (km/s) | Density (kg/m³) | Young's Modulus (MPa) | Poisson's Ratio | |-----------|------------------------|-----------------------|-----------------|
IS 13372 Part 1: Calculations & Interpretation of Results
| Parameter | Formula | Notes |
|---|---|---|
| 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 |
| Depth (m) | Density (×10³ kg/m³) | (V_p) (km/s) | (V_s) (km/s) | Poisson's Ratio | (E_d) (MPa) | (G) (MPa) |
|---|---|---|---|---|---|---|
| 10 | 1.7 | 1.6 | 0.75 | 0.359 | 2650 | 980 |
| 30 | 2.4 | 3.0 | 1.4 | 0.361 |
IS 13372 Part 1: Reporting of Results - Key Points
The test report must include:
Given:
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)} ]
| Depth (m) | Density (×10³ kg/m³) | (V_p) (km/s) | (V_s) (km/s) | Poisson's Ratio ((\mu)) | (G_d) (MPa) | (E_d) (MPa) |
|---|---|---|---|---|---|---|
| 10 | 1.7 | 1.6 | 0.75 | 0.359 | 980 | 2650 |
| 20-30 | 2.4 | 3. |
IS 13372 Part 1 covers Quality Control and Accuracy for surveying instruments.
| Instrument Type | Angular Accuracy (seconds) | Distance Accuracy (mm + ppm × D) |
|---|---|---|
| Theodolite | ±5 to ±20 | N/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.
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.
| Wave Type | Surface Source Examples | Borehole Source Examples |
|---|---|---|
| P wave | Explosives, sledgehammer, falling weight | Explosives, sparker, air gun, hammering device |
| SH wave | Plank hammering, SH gun, horizontal vibrator | Horizontal hammering device, vibrator |
| SV wave | Sledgehammer, falling weight | Explosives, 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
Frequently Asked
According to IS 13372 Part 1 (1992):
These waves are essential for determining velocity distribution, elastic moduli, and geotechnical interpretation.
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This measurement enables calculation of dynamic elastic moduli and soil/rock properties per IS 13372 Part 1.
Recommended Seismic Sources and Receivers for Downhole Seismic Testing (IS 13372 Part 1):
| Receiver Type | Signal Measured | Frequency Range | Notes |
|---|---|---|---|
| Geophone | Particle velocity | 10 Hz – 2 kHz | Natural freq. < 0.5 × predominant seismic freq. |
| Piezoelectric Accelerometer | Particle acceleration | 10 Hz – 60 kHz | Natural freq. ≥ 2 × predominant seismic freq. |
| Hydrophone | Pressure (water only) | 10 Hz – 60 kHz | Only for water-filled boreholes |
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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.
Seismic wave travel times are fundamental in calculating rock mechanical properties as per IS 13372 Part 1:
| Parameter | Formula |
|---|---|
| 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 | |
| ] |
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This approach provides a non-destructive, in-situ
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:
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Summary: Always generate and measure seismic waves after each relocation to ensure data accuracy, with special attention to SH waves for S-wave tests.
To comply with IS 13372 Part 1 for documenting and reporting test results:
The report must include:
| Item | Description |
|---|---|
| Borehole info | Location, dimensions, casing details |
| Seismic setup | Source/receiver positions & coordinates |
| Equipment & methods | Specs, frequency response, deviations |
| Data presentation | Waveforms, time-distance curves |
| Logs & velocities | Drilling log, velocity profiles |
| Computed parameters | Dynamic elastic modulus values |
| Analysis details | Equations, assumptions |
| Interpretation | Geotechnical context (if required) |
This ensures clarity, traceability, and compliance with IS 13372 Part 1.
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