IS 2720 Part 34 (1972) specifies the procedure for determining the in-place density of compacted or firmly bonded soils using the rubber-balloon method. This test method is essential for geotechnical engineers and construction professionals to assess soil compaction quality, bearing capacity, and stability of natural slopes. It is not suitable for very soft soils that deform easily. The standard details apparatus calibration, test hole volume measurement, and calculations to accurately determine soil density on site.
Overview
IS 2720 Part 34 (1972) specifies the procedure for determining the in-place density of compacted or firmly bonded soils using the rubber-balloon method. This test method is essential for geotechnical engineers and construction professionals to assess soil compaction quality, bearing capacity, and stability of natural slopes. It is not suitable for very soft soils that deform easily. The standard details apparatus calibration, test hole volume measurement, and calculations to accurately determine soil density on site.
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Structure
IS 2720 Part 34 - Scope: Key Formulas, Tables, and Specifications
| Temperature (°C) | Volume of Water (ml/g) |
|---|---|
| 12 | 1.00048 |
| 20 | 1.00177 |
| 30 | 1.00435 |
| 40 | 1.00786 |
| 50 | 1.01204 |
Volume varies slightly with temperature; important for precise moisture content calculations.
| Max Particle Size (mm) | Test Hole Volume (cm³) | Moisture Content Sample (g) |
|---|---|---|
| 4.75 | 700 | 200 |
| 10 | 1400 | 300 |
| 20 | 2100 | 500 |
| 40 | 2800 | 1000 |
| 63 | 3800 | 1500 |
Test hole size depends on particle size; larger holes improve accuracy.
flowchart TD
A[Test Hole Preparation] --> B[Dig Hole (Min Volume per Table 2)]
B --> C[Collect Soil Sample (Min Weight per Table 2)]
C --> D[Store Soil Airtight]
D --> E[Determine Moisture Content & Weight]
This concise scope ensures accurate field moisture testing per IS 2720 Part 34.
IS 2720 Part 34 (1972) Key References & Tables
| Temperature (°C) | Volume of Water (ml/g) |
|---|---|
| 12 | 1.00048 |
| 20 | 1.00177 |
| 30 | 1.00435 |
| 40 | 1.00786 |
| 50 | 1.01204 |
Use this table for precise water volume corrections at different temperatures during moisture content determinations.
| Max Particle Size (mm) | Test Hole Volume (cm³) | Moisture Content Sample (g) |
|---|---|---|
| 4.75 | 700 | 200 |
| 10 | 1400 | 300 |
| 20 | 2100 | 500 |
| 40 | 2800 | 1000 |
| 63 | 3800 | 1500 |
Larger holes improve accuracy; dimensions relate to apparatus and pressure used.
[ \gamma_d = \frac{w}{1 + \frac{w}{100}} \times \rho_w ]
Where:
Note: The clause gives a simplified formula to calculate dry unit weight from moisture content and wet weight.
If needed, I can provide a flow diagram of the field test procedure. Would you like that?
IS 2720 Part 34: Apparatus Key Points
| Temp (°C) | Volume of Water (ml/g) |
|---|---|
| 20 | 1.00177 |
| 25* | ~1.003 (interpolated) |
| 30 | 1.00435 |
| 40 | 1.00786 |
| 50 | 1.01204 |
*Use interpolation for intermediate temps.
| Max Particle Size (mm) | Min Test Hole Volume (cm³) | Min Moisture Sample (g) |
|---|---|---|
| 4.75 | 700 | 200 |
| 10 | 1,400 | 300 |
| 20 | 2,100 | 500 |
| 40 | 2,800 | 1,000 |
| 63 | 3,800 | 1,500 |
flowchart LR
A[Calibrated Vessel] --> B[Flexible Membrane (Rubber Balloon)]
B --> C[Test Hole in Soil]
A --> D[Volume Indicator]
A --> E[Pressure/Vacuum Control
IS 2720 Part 34: Key Test Procedure Details
| Max Particle Size (mm) | Test Hole Volume (cm³) | Moisture Content Sample (g) |
|---|---|---|
| 4.75 | 700 | 200 |
| 10 | 1,400 | 300 |
| 20 | 2,100 | 500 |
| 40 | 2,800 | 1,000 |
| 63 | 3,800 | 1,500 |
| Temperature (°C) | Volume of Water (ml/g) |
|---|---|
| 20 | 1.00177 |
| 30 | 1.00435 |
| 40 | 1.00786 |
| 50 | 1.01204 |
flowchart TD
A[Prepare Test Site] --> B[Set Apparatus & Record Initial Reading]
B --> C[Dig Test Hole (Volume per Table 2)]
C --> D[Collect Soil Sample for Moisture Content]
D --> E[Perform Volume & Pressure Measurements]
E --> F[Calculate & Report Results (Use Table 1 for Water Volume)]
This ensures accurate in-situ volume and moisture content measurement per IS 2720 Part 34.
IS 2720 Part 34 — Key Formulas, Tables & Specifications for Calculations
Use Table 1 to find the volume of water (ml/g) at the observed temperature to calculate container volume:
| Temperature (°C) | Volume of Water (ml/g) |
|---|---|
| 20 | 1.00177 |
| 25 (approx.) | ~1.003 (interpolated) |
| 30 | 1.00435 |
| 40 | 1.00786 |
| 50 | 1.01204 |
Formula:
[ \text{Volume of container (ml)} = \text{Weight of water (g)} \times \text{Volume of water (ml/g at temp.)} ]
Calculate dry unit weight (Y_d) (g/cm³) of soil removed from test hole:
[ Y_d = \frac{W}{V} \times \frac{100}{100 + w} ]
Where:
Note: Clause 5.3 in the context gives a partial formula; the standard formula is as above.
| Max Particle Size (mm) | Min Test Hole Volume (cm³) | Min Moisture Sample (g) |
|---|---|---|
| 4.75 | 700 | 200 |
| 10 | 1400 | 300 |
| 20 | 2100 | 500 |
| 40 | 2800 | 1000 |
| 63 | 3800 | 1500 |
flowchart TD
A[Determine weight of water in container] --> B[Measure water temperature]
B --> C[Find volume of water per gram from Table 1]
IS 2720 Part 34: Accuracy & Limitations Key Points
Volume of water varies with temperature; use Table 1 for precise volume conversion (ml/g).
Formula to calculate container volume:
[ V = W \times V_w(T) ]
Where:
| Temperature (°C) | Volume of Water (ml/g) |
|---|---|
| 20 | 1.00177 |
| 30 | 1.00435 |
| 40 | 1.00786 |
| 50 | 1.01204 |
| Max Particle Size (mm) | Test Hole Volume (cm³) | Moisture Sample Weight (g) |
|---|---|---|
| 4.75 | 700 | 200 |
| 10 | 1,400 | 300 |
| 20 | 2,100 | 500 |
| 40 | 2,800 | 1,000 |
| 63 | 3,800 | 1,500 |
flowchart TD
A[Fill container with water] --> B[Weigh water (W)]
B --> C[Measure water temperature (T)]
C --> D[Look up volume per gram Vw(T) from Table 1]
D --> E[Calculate container volume V = W × Vw(T)]
E --> F[Repeat 3 times; variation ≤ 3 ml]
F --> G[Use volume
IS 2720 Part 34: Reporting of Results - Key Formulas & Tables
Rounding Off Results
Volume of Water per Gram (Table 1, Clause 3.1.1)
Volume varies with temperature (ºC):
| Temperature (ºC) | Volume of Water (ml/g) |
|---|---|
| 12 | 1.00048 |
| 20 | 1.00177 |
| 30 | 1.00435 |
| 40 | 1.00786 |
| 50 | 1.01204 |
| Max Particle Size (mm) | Test Hole Volume (cm³) | Moisture Content Sample (g) |
|---|---|---|
| 4.75 | 700 | 200 |
| 10 | 1400 | 300 |
| 20 | 2100 | 500 |
| 40 | 2800 | 1000 |
| 63 | 3800 | 1500 |
Summary:
Report results rounded per IS 2-1960, use temperature-dependent water volume values, and ensure minimum test hole volumes and moisture samples based on particle size for reliable soil testing.
IS 2720 Part 34 (1972) – Notes and Precautions
| Temperature (°C) | Volume of Water (ml/g) |
|---|---|
| 12 | 1.00048 |
| 14 | 1.00073 |
| 16 | 1.00103 |
| 18 | 1.00138 |
| 20 | 1.00177 |
| 22 | 1.00221 |
| 24 | 1.00268 |
| 26 | 1.00320 |
| 28 | 1.00375 |
| 30 | 1.00435 |
| 32 | 1.00497 |
| 34 | 1.00563 |
| 36 | 1.00633 |
| 38 | 1.00706 |
| 40 | 1.00786 |
| 42 | 1.00857 |
| 44 | 1.00939 |
| 46 | 1.01031 |
| 48 | 1.01112 |
| 50 | 1.01204 |
This table and notes ensure accurate water volume correction in soil testing, critical for consistency in compaction and moisture content determination.
Frequently Asked
The rubber-balloon method (IS 2720 Part 34) is primarily suitable for cohesive soils and fine-grained soils where a small test hole can be made without significant disturbance.
| Soil Type | Suitability for Rubber-Balloon Method |
|---|---|
| Clay & Silts | Suitable |
| Sands & Gravels | Generally Not Suitable |
This method is best for in-situ density measurement of cohesive soils with minimal disturbance.
Calibration of Rubber-Balloon Apparatus (IS 2720 Part 34)
Fill apparatus with water to the required level; place on smooth horizontal surface and record initial volume reading.
Transfer apparatus to a calibrated container (simulating test hole volume). Inflate balloon to completely fill container, removing air bubbles by kneading membrane (Note 3).
Apply pressure until volume reading stabilizes; record final volume and pressure. Add weights (surcharge) if apparatus tends to rise (Note 4).
Calculate indicator volume value:
[
\text{Indicator Volume} = \text{Final reading} - \text{Initial reading}
]
Withdraw membrane by applying partial vacuum; repeat for containers of different sizes covering test hole range.
Accuracy requirement: Volume measurement must be within ±1% of known container volume.
Key Points:
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This ensures precise volume measurement for soil density testing.
To measure the volume of a test hole accurately as per IS 2720 Part 34, follow these key steps:
Prepare the Test Hole Surface (Clause 4.1):
Inflate the Flexible Membrane (Clause 4.3):
Post-Test Procedure:
Calibration & Accuracy (Clause 3.1 & 2.1):
| Step | Key Action | Notes |
|---|---|---|
| Surface Preparation | Plane surface, initial reading | Record pressure, surcharge |
| Membrane Inflation | Inflate membrane, avoid trapped air | Use same pressure/surcharge |
| Volume Measurement | Record volume difference, temperature correct | Volume = Final - Initial reading |
| Calibration | Check accuracy with standard molds | ±1% accuracy required |
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This ensures precise volume measurement of test holes in soils.
Effect of Temperature Variations on Volume Measurements (IS 2720 Part 34)
The volume of water used to fill calibration containers depends on water density, which varies with temperature.
Measure water temperature during volume determination.
Use Table 1 from Clause 3.1.1 to find the volume of water per gram (ml/g) at the observed temperature.
Calculate container volume as:
[ \text{Volume (ml)} = \text{Weight of water (g)} \times \text{Volume of water per gram (ml/g at measured temperature)} ]
Temperature correction is essential because water expands with temperature, affecting volume accuracy.
Calibration and test readings must be corrected for temperature differences between calibration and field conditions (Clause 4.3).
| Temperature (°C) | Volume of Water (ml/g) |
|---|---|
| 20 | 1.00177 |
| 25 (approx.) | ~1.00394 (interpolated) |
| 30 | 1.00435 |
| 40 | 1.00786 |
| 50 | 1.01204 |
Summary: Always record water temperature and apply the corresponding volume correction factor from the table to ensure precise volume measurements in soil testing.
Limitations of IS 2720 Part 34 (Rubber Balloon Method) vs. Sand Replacement Method (IS 2720 Part 28):
Soil Deformation Risk:
The rubber balloon method applies pressure on the liquid and surcharge weights that may deform weak or unsupported soils, causing inaccurate volume readings. Sand replacement does not induce such pressure.
Apparatus Sensitivity:
Requires careful calibration and pressure control to avoid errors. Sand replacement is more straightforward and less sensitive to apparatus calibration.
Accuracy in Weak Soils:
Balloon method may yield erroneous volume if soil collapses under pressure; sand replacement better for weak or loose soils.
Equipment Portability and Complexity:
Balloon method equipment is portable but requires careful handling of membrane and pressure control; sand replacement involves handling sand and excavation but is simpler.
Volume Measurement Precision:
Balloon method can achieve ~1% accuracy if properly calibrated; sand replacement is traditionally reliable but can be affected by sand compaction and moisture.
| Aspect | Rubber Balloon Method (IS 2720 Part 34) | Sand Replacement Method (IS 2720 Part 28) |
|---|---|---|
| Soil disturbance | Possible deformation under pressure | Minimal, sand fills hole directly |
| Calibration | Required for membrane & pressure control | Less critical, relies on sand volume |
| Suitability | Less suitable for weak/loose soils | Suitable for all soil types |
| Equipment complexity | Moderate (membrane, pressure system) | Simple (sand, container, scoop) |
| Accuracy | ~1% if careful | Generally reliable but depends on sand quality |
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In brief: Use the balloon method for firm soils with careful calibration; prefer sand replacement for weak or easily
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