IS 2720 Part 61972AI Search Enabled✦ AI Generated

Methods of test for soils, Part 6: Determination of shrinkage factors

IS 2720 Part 6 (1972) specifies the standardized laboratory methods for determining shrinkage factors of soils, including shrinkage limit, shrinkage ratio, and volumetric shrinkage. It provides detailed procedures for testing both remoulded and undisturbed soil samples using specified apparatus and calculation formulas. This standard is essential for geotechnical engineers and soil testing laboratories to assess soil volume changes due to moisture variation, critical for foundation design, earthworks, and soil stability analysis.

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What This Standard Covers

IS 2720 Part 6 (1972) specifies the standardized laboratory methods for determining shrinkage factors of soils, including shrinkage limit, shrinkage ratio, and volumetric shrinkage. It provides detailed procedures for testing both remoulded and undisturbed soil samples using specified apparatus and calculation formulas. This standard is essential for geotechnical engineers and soil testing laboratories to assess soil volume changes due to moisture variation, critical for foundation design, earthworks, and soil stability analysis.

Who Uses This Standard

  • Geotechnical Engineers
  • Soil Testing Laboratory Technicians
  • Civil Engineers
  • Foundation Design Specialists
  • Construction Material Inspectors
  • Research Scientists in Soil Mechanics
  • Irrigation and Land Reclamation Engineers

Key Topics Covered

Shrinkage limit determination for remoulded soil
Shrinkage limit determination for undisturbed soil
Shrinkage ratio calculation
Volumetric shrinkage measurement
Preparation and handling of soil samples
Use of mercury displacement method
Apparatus specifications including shrinkage dish and glass plates
Test procedure and step-by-step methodology
Calculation formulas for shrinkage factors
Reporting and recording test results
Definitions of key soil shrinkage terms
Sample preparation and drying techniques

Table of Contents

1Scope

IS 2720 Part 6: Scope - Key Points

  • Scope: This part of IS 2720 covers the determination of shrinkage factors of soils, essential for volume change calculations in geotechnical design.

  • Definitions: Refer to IS 2809-1972 for terms not defined here.

  • Referenced Standards:

    • IS 2720 Part III Section 2 (1980) for specific gravity determination of fine, medium, and coarse-grained soils.
    • Equipment specifications for shrinkage factor determination are also included.
  • Formula for Shrinkage Factor (Clause 5.4):

    [ S = \frac{V_w - V_d}{V_w} ]

    Where:

    • ( S ) = Shrinkage factor
    • ( V_w ) = Volume of wet soil
    • ( V_d ) = Volume of dry soil
  • International Coordination: The standard aligns with international practices while considering Indian field conditions.


Summary Table: Key References

ClauseContentReference Standard
2.1DefinitionsIS 2809-1972
7.6Specific gravity test methodIS 2720 Part III/Sec 2 (1980)
5.4Shrinkage factor formulaIS 2720 Part 6
flowchart LR
    A[Soil Sample] --> B[Determine Volume of Wet Soil (Vw)]
    B --> C[Dry Soil Sample]
    C --> D[Determine Volume of Dry Soil (Vd)]
    D --> E[Calculate Shrinkage Factor S = (Vw - Vd)/Vw]

This concise overview helps understand the scope and key formulas in IS 2720 Part 6.

2Definitions

IS 2720 Part 6: Definitions - Key Points

  • Clause 2.1: Definitions used in this standard refer primarily to IS:2809-1972 for terms not explicitly defined here.

  • General Scope: This part deals with determination of shrinkage factors of soils.

  • Related Standards:

    • IS:2720 Part III/Section 2 (1980) is the updated reference for specific gravity determination of soils (fine, medium, coarse).
    • Equipment specifications for shrinkage factor tests are also referenced.

Important Definitions (from IS 2809 and IS 2720 Part 6 context):

TermDefinition Summary
Shrinkage FactorRatio of volume change to the volume of solids.
Specific GravityRatio of unit weight of soil solids to unit weight of water.
Dry DensityMass of dry soil per unit volume of soil.

Key Formula for Shrinkage Factor (from Clause 5.4):

[ S = \frac{V_w - V_d}{V_s} ]

Where:

  • ( S ) = Shrinkage factor
  • ( V_w ) = Volume of wet soil
  • ( V_d ) = Volume of dry soil
  • ( V_s ) = Volume of solids

Notes:

  • The standard emphasizes international coordination and local practice relevance.
  • Use IS 2720 Part III/Section 2 (1980) for specific gravity tests.
  • Equipment specifications are detailed for shrinkage factor determination.

flowchart LR
    A[Soil Sample] --> B[Determine Volume of Wet Soil (Vw)]
    B --> C[Dry Soil Sample]
    C --> D[Determine Volume of Dry Soil (Vd)]
    A --> E[Determine Volume of Solids (Vs)]
    B & D & E --> F[Calculate Shrinkage Factor S = (Vw - Vd)/Vs]

This concise summary should help clarify definitions and related formulae in IS 2720 Part 6.

3Apparatus

IS 2720 Part 6 — Apparatus Specifications

Key Apparatus Dimensions & Details (Clause 3.6)

  • Glass Plates: Two plates, each 75 mm x 75 mm, thickness 3 mm
    • One plain glass plate
    • One glass plate with 3 metal prongs (inert to mercury)
  • Other Apparatus:
    • Evaporating dish, spatula, shrinkage dish, straight edge, glass cup, prong plate, plain plate, measuring cylinder per IS 10077-1982

Apparatus Purpose

  • Used for determining volumetric changes in soil by measuring mercury displacement.

Key Notes:

  • Metal prongs help hold soil pat firmly.
  • Mercury displacement method is used to measure volume change before and after shrinkage.

Summary Table of Apparatus Dimensions

Apparatus ComponentDimensions/Specification
Glass Plates75 mm × 75 mm × 3 mm thickness
Metal Prongs3 prongs, inert to mercury
Evaporating Dish & OthersAs per IS 10077-1982

Visual Concept (simplified):

flowchart LR
    SoilPat[Soil Pat on Glass Plate]
    GlassPlate1[Plain Glass Plate]
    GlassPlate2[Glass Plate with Metal Prongs]
    Mercury[Mercury in Evaporating Dish]
    
    SoilPat --> GlassPlate2
    GlassPlate2 --> Mercury
    Mercury --> VolumeChange[Measure Displaced Mercury]

This setup allows precise volumetric shrinkage measurement by mercury displacement.


For detailed apparatus specs, refer to IS 10077-1982 and IS 2720 Part 6 (Clause 3.6).

4Soil Sample for Test

IS 2720 Part 6 — Soil Sample for Test: Key Points

Sampling & Testing Procedure

  • Clause 8.2:
    • Perform minimum 3 tests per soil sample.
    • Calculate the average of results.
    • Discard any test result differing by ±2% from the average and retest.

Specific Gravity

  • Clause 6.3:

    • Determine Specific Gravity (G) as per IS 2720 Part 3 (1964).
    • Typically, use the formula:

    [ G = \frac{\text{Weight of soil solids}}{\text{Weight of equal volume of water}} ]

Equipment & Conditions

  • Clause 3.11:
    • Use a desiccator with a desiccating agent (other than sulphuric acid) for moisture control.

Summary Table: Test Repetition Criteria

Test No.Result (%)Action
1x1Record
2x2Record
3x3Record
Avg(x1+x2+x3)/3Calculate
CheckIf anyx_i - Avg

Notes:

  • Repeat tests ensure accuracy and reliability of soil properties.
  • Specific gravity is essential for further calculations like void ratio, porosity, and degree of saturation.
flowchart TD
    A[Soil Sample] --> B[Perform 3 Tests]
    B --> C{Check Variation ±2%?}
    C -- Yes --> D[Discard Outlier]
    D --> B
    C -- No --> E[Calculate Average]
    E --> F[Report Results]

This ensures consistent and reliable soil characterization per IS 2720 Part 6.

5Procedure for Determination of Shrinkage Limit (Remoulded Soil) and Allied Properties

IS 2720 Part 6: Shrinkage Limit (Remoulded Soil) - Key Points

Sample Preparation

  • Use 100 g of soil passing 425 micron IS sieve (Clause 4.1).
  • Prepare soil pats of 45 mm diameter and 15 mm height (Clause 4.2.2).
  • Round edges to avoid air entrapment during mercury displacement.

Shrinkage Limit (Remoulded Soil), ( w_s )

  • Calculated by:

[ w_s = \frac{W_s - W_d}{W_d} \times 100 ]

Where:

  • ( W_s ) = Weight of water in the soil at shrinkage limit
  • ( W_d ) = Weight of dry soil solids

Allied Properties Calculated

  • Shrinkage Ratio (Sr)
  • Shrinkage Index (Is)
  • Volumetric Shrinkage (Vs)

Typical Procedure Summary

flowchart TD
    A[Sample Preparation] --> B[Weigh Soil]
    B --> C[Form Soil Pats]
    C --> D[Dry Soil Pats]
    D --> E[Measure Volume & Weight]
    E --> F[Calculate Shrinkage Limit]
    F --> G[Calculate Allied Properties]

For detailed formulas of allied properties, refer to IS 2720 Part 6 Clauses 7.3-7.5.

6Procedure for Determination of Shrinkage Limit (Undisturbed Soil)

IS 2720 Part 6: Procedure for Determination of Shrinkage Limit (Undisturbed Soil)


Sample Preparation (Clause 4.2.2)

  • Trim undisturbed soil pats:
    • Diameter ≈ 45 mm
    • Height ≈ 15 mm
  • Round edges to avoid air entrapment during mercury displacement.

Mercury Displacement Method (Clause 5.5.1)

  • Fill glass cup with mercury, remove excess using a glass plate with three prongs.
  • Place oven-dried soil pat on mercury surface, gently press under mercury using the plate.
  • Weigh displaced mercury to 0.1 g accuracy.
  • Calculate volume of oven-dried soil pat:
    [ V_o' = \frac{\text{Weight of displaced mercury}}{\text{Unit weight of mercury}} ]

Shrinkage Limit Calculation (Clause 7.6)

[ W_{su} = \frac{(W_{os} - W_{od}) \times V_{os}}{V_o'} \times 100 ]

Where:

  • (W_{su}) = Shrinkage limit of undisturbed soil (%)
  • (W_{os}) = Water content of soil sample before drying (%)
  • (W_{od}) = Water content of oven-dried soil (usually 0%)
  • (V_{os}) = Volume of soil sample before drying (mercury displacement)
  • (V_o') = Volume of oven-dried soil pat (mercury displacement)

Summary Table

ParameterTypical Value / Unit
Soil pat diameter45 mm
Soil pat height15 mm
Mercury unit weight13.6 g/cm³
Volume measurement accuracy±0.1 g mercury weight

flowchart TD
    A[Trim Soil Pat (45mm x 15mm)] --> B[Place on Mercury]
    B --> C[Press Pat Under Mercury]
    C --> D[Measure Displaced Mercury Weight]
    D --> E[Calculate Volume of Oven-Dried Soil Pat]
    E --> F[Calculate Shrinkage Limit using formula]

This procedure ensures accurate measurement of shrinkage limit

7Calculation of Shrinkage Factors

IS 2720 Part 6: Calculation of Shrinkage Factors

Key Definitions & Formulas

  • Shrinkage Limit, ws (%): Water content below which soil ceases to shrink.

  • Shrinkage Ratio, R (Clause 2.1.4):
    [ R = \frac{\text{Volume change } (%) \text{ w.r.t dry volume}}{\text{Change in water content } (%) \text{ above } w_s} ]

  • Volumetric Shrinkage (V₃) (Clause 7.5):
    [ V_3 = (w_1 - w_s) \times R ] where:

    • ( w_1 ) = initial water content (%)
    • ( w_s ) = shrinkage limit (%)
    • ( R ) = shrinkage ratio
  • Specific Gravity, G: Determined as per IS 2720 Part 3.


Summary Table for Shrinkage Parameters

ParameterSymbolUnit/DescriptionReference Clause
Shrinkage Limit( w_s )% water content where shrinkage stops7.4
Shrinkage Ratio( R )Volume change per unit water content change2.1.4
Volumetric Shrinkage( V_3 )% volume change due to drying7.5
Specific Gravity( G )Unitless, soil solids density ratioIS 2720 Part 3

Notes:

  • The shrinkage ratio ( R ) is dimensionless.
  • ( V_3 ) gives volumetric shrinkage relative to dry soil volume.
  • Use oven-dried soil weight as basis for water content changes.
flowchart TD
    A[Initial Water Content \(w_1\)] --> B[Subtract Shrinkage Limit \(w_s\)]
    B --> C[Multiply by Shrinkage Ratio \(R\)]
    C --> D[Volumetric Shrinkage \(V_3\)]

This concise framework allows calculation of volumetric shrinkage from measured water contents and shrinkage limits per IS

8Reporting of Results

IS 2720 Part 6: Reporting of Results - Key Points

  • Test Repetition & Averaging (Clause 8.2):

    • Perform at least 3 tests per soil sample.
    • Calculate the average of the results.
    • Discard any test result differing by ±2% or more from the average and repeat the test.
  • Rounding Off (Clause 0.5):

    • Round off final values as per IS 2-1960 guidelines (generally to the nearest significant digit).
  • Record Format (Clause 8.1):

    • Use the pro forma in Appendix A for uniform reporting of observations and results.

Recommended Formula for Average Water Content (Example from Clause 5.4)

[ w = \frac{W_w}{W_s} \times 100 ]

Where:

  • (w) = water content (%)
  • (W_w) = weight of water
  • (W_s) = weight of dry soil

Summary Table for Reporting

StepRequirement
Number of TestsMinimum 3 per sample
Acceptable Variation± 2% from average
RoundingAs per IS 2-1960
Documentation FormatAppendix A pro forma

flowchart TD
    A[Start Testing] --> B{Perform 3 Tests}
    B --> C[Calculate Average]
    C --> D{Any value ±2% from Average?}
    D -- Yes --> E[Discard & Repeat Test]
    D -- No --> F[Report Average]
    F --> G[Round off as per IS 2-1960]
    G --> H[Record in Appendix A format]
    H --> I[End]

This ensures accuracy, consistency, and clarity in soil water content reporting under IS 2720 Part 6.

Appendix APro Forma for Record of Test Results

IS 2720 Part 6: Pro Forma for Record of Test Results (Appendix A)

  • Test Reporting Requirements (Clause 8.1 & 8.2):

    • Perform minimum 3 tests per soil sample.
    • Calculate the average of results.
    • Discard any value deviating by ±2% from the average; repeat test if needed.
    • Round off final values as per IS 2-1960 rounding rules.
  • Pro Forma Elements (Appendix A) typically include:

    • Sample Identification: Location, depth, date.
    • Test Details: Type of test, apparatus used, date of test.
    • Observations: Water content, weight measurements, volume, etc.
    • Calculations: Bulk density, dry density, water content.
    • Results: Individual test values, average value.
    • Remarks: Any anomalies or observations during testing.
  • Key Formula for Dry Density (Clause 5.4 reference):

[ \text{Dry Density} (\rho_d) = \frac{\text{Bulk Density} (\rho)}{1 + w} ]

Where:

  • ( \rho ) = Bulk density (mass/volume)
  • ( w ) = Water content (decimal)

Summary Table for Test Result Reporting

ParameterDetails/UnitsRemarks
Sample IDTextLocation, depth, date
Bulk Density ((\rho))g/cm³ or kN/m³Measured
Water Content (w)% or decimalMeasured
Dry Density ((\rho_d))g/cm³ or kN/m³Calculated
Individual Test ValuesNumericAt least 3 readings
Average ValueNumericMean of valid test results
Observations/RemarksTextDeviations, equipment used

flowchart TD
    A[Soil Sample Collection] --> B[Conduct 3 Tests]
    B --> C{Check Variation ±2%}
    C -- Within Limit --> D[Calculate Average]
    C -- Exceeds Limit --> B
    D --> E[Round Off Values (

Popular Questions About IS 2720 Part 6

?What apparatus is required for determining the shrinkage limit according to IS 2720 Part 6?

According to IS 2720 Part 6, the apparatus required for determining the shrinkage limit includes:

  • Glass cup (with a flat top)
  • Glass plate with three prongs (to press the soil pat and remove excess mercury)
  • Mercury (to measure volume displacement)
  • Evaporating dish (to collect displaced mercury)
  • Balance (accurate to 0.1 g for weighing mercury displaced)
  • Oven (for drying soil pats)
  • Soil pat molds (to prepare soil samples of approx. 45 mm diameter and 15 mm height)
  • 425-micron IS sieve (for sample preparation)

Key steps involving apparatus:

  • Fill the glass cup with mercury.
  • Place the oven-dried soil pat on mercury.
  • Press with the three-pronged glass plate to displace mercury.
  • Measure displaced mercury weight to find soil pat volume.

This mercury displacement method is essential to determine the volume of the dry soil pat accurately.

Loading diagram...

This setup ensures precise volume measurement critical for shrinkage limit determination.

?How is the shrinkage limit of remoulded soil different from that of undisturbed soil?

Difference between Shrinkage Limit of Remoulded and Undisturbed Soil (IS 2720 Part 6):

  • Shrinkage Limit (Undisturbed Soil) (wsu):
    The maximum water content at which further drying does not reduce the volume of the soil mass in its natural, undisturbed state (Clause 2.1.2).

  • Shrinkage Limit (Remoulded Soil) (ws):
    The maximum water content at which further drying does not reduce the volume of the soil mass prepared from remoulded (disturbed) soil passing 425-micron sieve (Clause 2.1.3 & 4.1).

Key Differences:

  • Sample State:

    • Undisturbed soil: Natural structure preserved.
    • Remoulded soil: Soil is disturbed, mixed, and passed through 425-micron sieve.
  • Volume Change Behavior:

    • Undisturbed soil shrinkage limit reflects natural fabric and structure.
    • Remoulded soil shrinkage limit reflects behavior after soil structure is destroyed.

Practical Implication:

  • Shrinkage limit of remoulded soil is usually higher because the soil fabric is broken, allowing more volume change before reaching zero shrinkage.

Loading diagram...

Summary:
Shrinkage limit depends on soil structure; undisturbed soil reflects in-situ conditions, remoulded soil reflects disturbed conditions with typically higher shrinkage limits.

?What is the procedure for measuring volumetric shrinkage using mercury displacement?

Procedure for Measuring Volumetric Shrinkage Using Mercury Displacement (IS 2720 Part 6):

  1. Prepare Soil Pat:

    • Trim an oven-dried soil pat approx. 45 mm diameter × 15 mm height with rounded edges (Clause 4.2.2).
  2. Measure Volume of Oven-Dry Soil Pat (V'o):

    • Fill a glass cup with mercury to overflowing.
    • Remove excess mercury by pressing a glass plate with three prongs firmly on top (Clause 5.5.1).
    • Place the cup in an evaporating dish.
    • Place the oven-dried soil pat on mercury surface.
    • Press the soil pat under mercury using the glass plate with prongs, collecting displaced mercury.
    • Weigh displaced mercury to 0.1 g accuracy.
    • Calculate volume:
      [ V'_o = \frac{\text{Weight of displaced mercury}}{\text{Unit weight of mercury}} ]
  3. Measure Volume of Wet Soil Pat (V):

    • Use a shrinkage dish (45 mm diameter × 15 mm height, rounded corners) (Clause 3.3).
    • Fill dish with mercury to overflowing.
    • Remove excess mercury using a plain glass plate pressed firmly flush (no air entrapment).
    • Weigh mercury held in the dish.
    • Calculate volume:
      [ V = \frac{\text{Weight of mercury in dish}}{\text{Unit weight of mercury}} ]
  4. Volumetric Shrinkage Calculation: [ \text{Volumetric Shrinkage} = \frac{V - V'_o}{V} \times 100% ]


Notes:

  • Unit weight of mercury ≈ 13.6 g/cm³.
  • Ensure no air bubbles trapped under soil pat during mercury displacement.
  • Use accurate weighing scales (0.1 g precision).
Loading diagram...
?How should soil samples be prepared and handled for accurate shrinkage testing?

For accurate shrinkage limit testing per IS 2720 Part 6, follow these key steps for soil sample preparation and handling:

Sample Preparation (Clause 4.2.2 & 4.1)

  • Undisturbed Soil: Trim soil pats approx. 45 mm diameter × 15 mm height; round edges to avoid air entrapment during mercury displacement.
  • Remoulded Soil: Use about 100 g of soil passing through a 425-micron IS sieve, thoroughly mixed.

Handling for Shrinkage Limit Test

For Undisturbed Soil (Clause 5.3)

  • Coat shrinkage dish inside with silicone grease/vaseline to prevent soil adhesion.
  • Place soil paste equal to ~1/3 volume of dish, tap gently on cushioned surface to remove air.
  • Add soil in portions, tapping until dish is full and excess soil stands above edges.
  • Strike off excess soil and clean dish exterior.

Mercury Displacement (Clause 5.5.1)

  • Fill glass cup with mercury, remove excess with pronged glass plate.
  • Place oven-dried soil pat on mercury surface, press under mercury carefully to avoid air bubbles.
  • Collect displaced mercury, weigh to 0.1 g accuracy.
  • Calculate soil pat volume ( V_o' = \frac{\text{weight of displaced mercury}}{\text{unit weight of mercury}} ).

Summary Table:

StepDimension / QuantityNotes
Soil pat size (undisturbed)45 mm dia × 15 mm heightRounded edges
Soil sample (remoulded)~100 g, passing 425-micron sieveThoroughly mixed
Shrinkage dish filling~1/3 volume incrementsTap to remove air, grease inside
Mercury displacementWeight to 0.1 g accuracyAvoid air entrapment

This ensures precise volume measurement critical for shrinkage limit determination.

?What formulas are used to calculate shrinkage ratio and volumetric shrinkage?

IS 2720 Part 6: Shrinkage Ratio and Volumetric Shrinkage

1. Shrinkage Ratio (R)

Defined as the ratio of volume change per unit water content loss above the shrinkage limit.

Formula:

[ R = \frac{V_o - V_s}{W_o - W_s} ]

Where:

  • (V_o) = Volume of oven-dried soil pat (ml)
  • (V_s) = Volume at shrinkage limit (ml)
  • (W_o) = Water content at saturation or initial state (%)
  • (W_s) = Shrinkage limit water content (%)

Alternatively, expressed as a percentage of dry volume change per % water content change.


2. Volumetric Shrinkage (V₃)

Calculated using:

[ V_3 = (w_1 - w_s) \times R ]

Where:

  • (w_1) = Initial water content (%)
  • (w_s) = Shrinkage limit water content (%)
  • (R) = Shrinkage ratio (dimensionless)

Summary:

ParameterSymbolUnit/DimensionDescription
Shrinkage RatioRDimensionlessVolume change per unit water loss
Volumetric ShrinkageV₃Percentage of volumeTotal volumetric shrinkage

Loading diagram...

This provides a clear method to quantify soil volume changes due to drying beyond the shrinkage limit.

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