IS 2720 Part 341972AI Search Enabled✦ AI Generated

Methods of test for soils, Part 34: Determination of density of soil in place by the rubber-balloon method

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.

8Sections
99Clauses Indexed
AI Search Ready
1972Edition
Soil and Foundation EngineeringCategory
Alternative search terms: IS 2720 Part 34 PDF, IS 2720 Part 34 pdf free download, IS 2720 Part 34 free download pdf, IS2720Part34 PDF, IS-2720-Part-34 PDF, IS 2720 Part 34 1972 PDF, IS 2720 Part 34:1972 PDF, IS 2720 Part 34-1972 PDF, IS 2720 Part 34 (1972) PDF, IS 2720 Part 34 1972 edition PDF, IS 2720 Part 34 edition 1972 PDF

What This Standard Covers

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.

Who Uses This Standard

  • Geotechnical Engineers
  • Soil Testing Laboratory Technicians
  • Civil Engineers
  • Construction Quality Control Inspectors
  • Foundation Design Engineers
  • Field Surveyors
  • Research Officers in Soil Mechanics

Key Topics Covered

Scope and applicability of the rubber-balloon method
Apparatus requirements and calibration procedures
Preparation and measurement of test holes
Volume measurement using rubber-balloon apparatus
Calculation of moisture content and dry density
Limitations for use on soft soils
Correction factors for temperature
Use of surcharge weights during testing
Comparison with other density determination methods
Accuracy and precision requirements
Field test procedures
Reporting and rounding off results

Table of Contents

1Scope

IS 2720 Part 34 - Scope: Key Formulas, Tables, and Specifications

1. Volume of Water per Gram Based on Temperature (Clause 3.1.1)

Temperature (°C)Volume of Water (ml/g)
121.00048
201.00177
301.00435
401.00786
501.01204

Volume varies slightly with temperature; important for precise moisture content calculations.


2. Minimum Field Test Hole Volumes & Moisture Sample Sizes (Clause 4.2)

Max Particle Size (mm)Test Hole Volume (cm³)Moisture Content Sample (g)
4.75700200
101400300
202100500
4028001000
6338001500

Test hole size depends on particle size; larger holes improve accuracy.


Notes:

  • Test holes must be carefully dug to avoid disturbing surrounding soil.
  • Soil removed is stored airtight for moisture and weight tests.
  • Dimensions relate to apparatus design and pressure used.
  • Refer to IS 2720 Part 7 (1980) & Part 8 (1983) for related procedures.

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.

2References

IS 2720 Part 34 (1972) Key References & Tables


1. Volume of Water per Gram Based on Temperature (Clause 3.1.1)

Temperature (°C)Volume of Water (ml/g)
121.00048
201.00177
301.00435
401.00786
501.01204

Use this table for precise water volume corrections at different temperatures during moisture content determinations.


2. Minimum Field Test Hole Volumes & Moisture Content Samples (Clause 4.2)

Max Particle Size (mm)Test Hole Volume (cm³)Moisture Content Sample (g)
4.75700200
101400300
202100500
4028001000
6338001500

Larger holes improve accuracy; dimensions relate to apparatus and pressure used.


3. Dry Unit Weight Calculation (Clause 5.3)

[ \gamma_d = \frac{w}{1 + \frac{w}{100}} \times \rho_w ]

Where:

  • (\gamma_d) = Dry unit weight (g/cm³)
  • (w) = Moisture content (%)
  • (\rho_w) = Unit weight of water (typically 1 g/cm³)

Note: The clause gives a simplified formula to calculate dry unit weight from moisture content and wet weight.


Additional Notes

  • Substitute references to IS 2720 (Part 7) and (Part 8) with the latest revisions (1980 and 1983 respectively).
  • For detailed procedures, apparatus design, and calibration, refer to relevant clauses in IS 2720 Part 34.

If needed, I can provide a flow diagram of the field test procedure. Would you like that?

3Apparatus

IS 2720 Part 34: Apparatus Key Points

1. Calibrated Vessel (Clause 2.1)

  • Contains liquid with a flexible elastic membrane (rubber balloon) to measure test hole volume.
  • Graduated to 5 ml accuracy.
  • Equipped to apply external pressure or partial vacuum.
  • Size/weight must not distort test hole; surcharge weights can be added if needed.
  • Membrane size must fill hole without wrinkles and withstand necessary pressures.

2. Volume of Water per Gram (Clause 3.1.1 - Table 1)

Temp (°C)Volume of Water (ml/g)
201.00177
25*~1.003 (interpolated)
301.00435
401.00786
501.01204

*Use interpolation for intermediate temps.

3. Minimum Test Hole Volumes & Moisture Samples (Clause 4.2 - Table 2)

Max Particle Size (mm)Min Test Hole Volume (cm³)Min Moisture Sample (g)
4.75700200
101,400300
202,100500
402,8001,000
633,8001,500

4. Calibration Check (Clause 3.1.2)

  • Fill apparatus with water, take initial volume reading.
  • Place membrane in container, inflate fully, note final volume.
  • Apply pressure until volume stabilizes; record pressure.
  • Add surcharge weights if apparatus tends to rise.
  • Volume difference = container volume.
  • Remove membrane by partial vacuum.
  • Repeat for all calibration containers.

Summary Diagram of Apparatus Setup:

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
4Test Procedure

IS 2720 Part 34: Key Test Procedure Details

Test Hole Preparation (Clause 4.1 & 4.2)

  • Dig a hole centered within the apparatus outline; avoid disturbing soil around the top edge.
  • Minimum hole volume depends on max particle size (Table 2).
  • Collect soil from hole in airtight container for moisture and weight tests.
  • Hole dimensions should match calibration check dimensions for accuracy.

Table 2: Minimum Field Test Hole Volumes & Moisture Sample

Max Particle Size (mm)Test Hole Volume (cm³)Moisture Content Sample (g)
4.75700200
101,400300
202,100500
402,8001,000
633,8001,500

Volume of Water per Gram by Temperature (Table 1, Clause 3.1.1)

Temperature (°C)Volume of Water (ml/g)
201.00177
301.00435
401.00786
501.01204

Procedure Summary:

  1. Prepare a plane test site.
  2. Set apparatus, record initial volume reading, pressure, surcharge.
  3. Dig hole per Table 2 volumes.
  4. Collect soil for moisture content.
  5. Use water volume correction per temperature (Table 1).
  6. Report results rounded per IS 2-1960.

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.

5Calculations

IS 2720 Part 34 — Key Formulas, Tables & Specifications for Calculations


1. Volume of Water per Gram (Clause 3.1.1)

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)
201.00177
25 (approx.)~1.003 (interpolated)
301.00435
401.00786
501.01204

Formula:

[ \text{Volume of container (ml)} = \text{Weight of water (g)} \times \text{Volume of water (ml/g at temp.)} ]


2. Dry Unit Weight of Soil (Clause 5.3)

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:

  • (W) = weight of moist soil (g)
  • (V) = volume of soil (cm³)
  • (w) = moisture content (%)

Note: Clause 5.3 in the context gives a partial formula; the standard formula is as above.


3. Minimum Field Test Hole Volumes & Moisture Sample (Clause 4.2, Table 2)

Max Particle Size (mm)Min Test Hole Volume (cm³)Min Moisture Sample (g)
4.75700200
101400300
202100500
4028001000
6338001500

Summary Diagram of Calculation Flow

flowchart TD
    A[Determine weight of water in container] --> B[Measure water temperature]
    B --> C[Find volume of water per gram from Table 1]
6Accuracy and Limitations

IS 2720 Part 34: Accuracy & Limitations Key Points

1. Volume of Water per Gram (Clause 3.1.1)

  • 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:

    • (V) = volume of container (ml)
    • (W) = weight of water to fill container (g)
    • (V_w(T)) = volume of water per gram at temperature (T) (from Table 1)
Temperature (°C)Volume of Water (ml/g)
201.00177
301.00435
401.00786
501.01204

2. Minimum Field Test Hole Volumes & Sample Sizes (Clause 4.2, Table 2)

Max Particle Size (mm)Test Hole Volume (cm³)Moisture Sample Weight (g)
4.75700200
101,400300
202,100500
402,8001,000
633,8001,500
  • Larger holes improve accuracy.
  • Hole size relates to apparatus design and pressure.

3. Reporting & Rounding (IS 2-1960)

  • Final values must be rounded as per IS 2-1960 guidelines.

Summary Flowchart of Procedure

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
7Reporting of Results

IS 2720 Part 34: Reporting of Results - Key Formulas & Tables

  1. Rounding Off Results

    • Follow IS 2-1960 for rounding off final observed or calculated values.
  2. Volume of Water per Gram (Table 1, Clause 3.1.1)
    Volume varies with temperature (ºC):

Temperature (ºC)Volume of Water (ml/g)
121.00048
201.00177
301.00435
401.00786
501.01204
  1. Minimum Field Test Hole Volumes & Moisture Content Samples (Table 2, Clause 4.2)
Max Particle Size (mm)Test Hole Volume (cm³)Moisture Content Sample (g)
4.75700200
101400300
202100500
4028001000
6338001500
  • Use larger holes for better accuracy.
  • Hole dimensions should match apparatus design and calibration.

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.

8Notes and Precautions

IS 2720 Part 34 (1972) – Notes and Precautions

Key Table: Volume of Water per Gram vs Temperature (Clause 3.1.1)

Temperature (°C)Volume of Water (ml/g)
121.00048
141.00073
161.00103
181.00138
201.00177
221.00221
241.00268
261.00320
281.00375
301.00435
321.00497
341.00563
361.00633
381.00706
401.00786
421.00857
441.00939
461.01031
481.01112
501.01204

Important Notes & Substitutions:

  • References updated for related IS codes:
    • IS 2720 (Part 7) updated from 1965 to 1980
    • IS 2720 (Part 8) updated from 1965 to 1983
    • IS 2720 (Part 28) updated from 1966 to 1974

Precautions:

  • Use the correct volume of water based on temperature for accurate soil testing.
  • Always refer to the latest IS codes for related procedures and corrections.
  • Ensure temperature measurement is precise as volume changes affect test results.

This table and notes ensure accurate water volume correction in soil testing, critical for consistency in compaction and moisture content determination.

Popular Questions About IS 2720 Part 34

?What types of soils is the rubber-balloon method suitable for?

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.

Suitability:

  • Fine-grained soils (clays, silts) where the hole walls remain stable.
  • Soils that do not collapse or cave in easily when a test hole is made.
  • Not ideal for coarse granular soils (sands, gravels) because the hole may collapse or the balloon may not fully expand to fill the irregular cavity.

Key Points:

  • The method involves measuring volume change by inflating a rubber balloon in a test hole.
  • Requires a stable hole to accurately measure the volume displaced.
  • Additional surcharge weights may be used to prevent the apparatus from rising, but this can induce soil deformation.

Summary:

Soil TypeSuitability for Rubber-Balloon Method
Clay & SiltsSuitable
Sands & GravelsGenerally Not Suitable

This method is best for in-situ density measurement of cohesive soils with minimal disturbance.

?How is the rubber-balloon apparatus calibrated before testing?

Calibration of Rubber-Balloon Apparatus (IS 2720 Part 34)

  1. Fill apparatus with water to the required level; place on smooth horizontal surface and record initial volume reading.

  2. Transfer apparatus to a calibrated container (simulating test hole volume). Inflate balloon to completely fill container, removing air bubbles by kneading membrane (Note 3).

  3. Apply pressure until volume reading stabilizes; record final volume and pressure. Add weights (surcharge) if apparatus tends to rise (Note 4).

  4. Calculate indicator volume value:
    [ \text{Indicator Volume} = \text{Final reading} - \text{Initial reading} ]

  5. Withdraw membrane by applying partial vacuum; repeat for containers of different sizes covering test hole range.

  6. Accuracy requirement: Volume measurement must be within ±1% of known container volume.


Key Points:

  • Use containers/moulds simulating actual test holes (100mm, 150mm diameters).
  • Apparatus must avoid distortion of test holes during calibration.
  • Pressure and vacuum applied via portable actuator bulb.
Loading diagram...

This ensures precise volume measurement for soil density testing.

?What are the key steps to measure the volume of a test hole accurately?

To measure the volume of a test hole accurately as per IS 2720 Part 34, follow these key steps:

  1. Prepare the Test Hole Surface (Clause 4.1):

    • Ensure the test hole surface is reasonably plane.
    • Place the calibrated apparatus on the hole.
    • Take an initial volume reading using the same pressure and surcharge weight as during calibration.
    • Scribe the apparatus outline and record pressure, surcharge, and initial reading.
  2. Inflate the Flexible Membrane (Clause 4.3):

    • Position the apparatus exactly as for the initial reading.
    • Inflate the membrane, allowing air to escape without trapping between membrane and hole surface.
    • Apply the same surcharge weight and pressure as calibration.
    • Record the volume reading; the difference from the initial reading is the test hole volume.
    • Correct volume for water temperature differences.
  3. Post-Test Procedure:

    • Pump water and membrane back into the cylinder by vacuum.
  4. Calibration & Accuracy (Clause 3.1 & 2.1):

    • Calibrate with containers simulating test holes to ensure ±1% accuracy.
    • Use flexible membranes sized to fill holes without wrinkles.
    • Adjust surcharge/pressure if soil deformation affects volume.

Summary Table

StepKey ActionNotes
Surface PreparationPlane surface, initial readingRecord pressure, surcharge
Membrane InflationInflate membrane, avoid trapped airUse same pressure/surcharge
Volume MeasurementRecord volume difference, temperature correctVolume = Final - Initial reading
CalibrationCheck accuracy with standard molds±1% accuracy required
Loading diagram...

This ensures precise volume measurement of test holes in soils.

?How do temperature variations affect the volume measurements?

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)
201.00177
25 (approx.)~1.00394 (interpolated)
301.00435
401.00786
501.01204

Summary: Always record water temperature and apply the corresponding volume correction factor from the table to ensure precise volume measurements in soil testing.

?What are the limitations of this method compared to the sand replacement method?

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.


Summary Table

AspectRubber Balloon Method (IS 2720 Part 34)Sand Replacement Method (IS 2720 Part 28)
Soil disturbancePossible deformation under pressureMinimal, sand fills hole directly
CalibrationRequired for membrane & pressure controlLess critical, relies on sand volume
SuitabilityLess suitable for weak/loose soilsSuitable for all soil types
Equipment complexityModerate (membrane, pressure system)Simple (sand, container, scoop)
Accuracy~1% if carefulGenerally reliable but depends on sand quality

Loading diagram...

In brief: Use the balloon method for firm soils with careful calibration; prefer sand replacement for weak or easily

Need Detailed Clause Answers?

Ask AI about any clause, requirement, or provision in IS 2720 Part 34. Get instant, clause-cited responses powered by our indexed library.

Free tier includes 150 queries (50 AI + 100 Reference) · No credit card required