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.
Overview
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.
Audience
Contents
Structure
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:
Formula for Shrinkage Factor (Clause 5.4):
[ S = \frac{V_w - V_d}{V_w} ]
Where:
International Coordination: The standard aligns with international practices while considering Indian field conditions.
| Clause | Content | Reference Standard |
|---|---|---|
| 2.1 | Definitions | IS 2809-1972 |
| 7.6 | Specific gravity test method | IS 2720 Part III/Sec 2 (1980) |
| 5.4 | Shrinkage factor formula | IS 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.
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:
| Term | Definition Summary |
|---|---|
| Shrinkage Factor | Ratio of volume change to the volume of solids. |
| Specific Gravity | Ratio of unit weight of soil solids to unit weight of water. |
| Dry Density | Mass of dry soil per unit volume of soil. |
[ S = \frac{V_w - V_d}{V_s} ]
Where:
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.
IS 2720 Part 6 — Apparatus Specifications
| Apparatus Component | Dimensions/Specification |
|---|---|
| Glass Plates | 75 mm × 75 mm × 3 mm thickness |
| Metal Prongs | 3 prongs, inert to mercury |
| Evaporating Dish & Others | As per IS 10077-1982 |
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).
IS 2720 Part 6 — Soil Sample for Test: Key Points
Clause 6.3:
[ G = \frac{\text{Weight of soil solids}}{\text{Weight of equal volume of water}} ]
| Test No. | Result (%) | Action |
|---|---|---|
| 1 | x1 | Record |
| 2 | x2 | Record |
| 3 | x3 | Record |
| Avg | (x1+x2+x3)/3 | Calculate |
| Check | If any | x_i - Avg |
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.
IS 2720 Part 6: Shrinkage Limit (Remoulded Soil) - Key Points
[ w_s = \frac{W_s - W_d}{W_d} \times 100 ]
Where:
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.
IS 2720 Part 6: Procedure for Determination of Shrinkage Limit (Undisturbed Soil)
[ W_{su} = \frac{(W_{os} - W_{od}) \times V_{os}}{V_o'} \times 100 ]
Where:
| Parameter | Typical Value / Unit |
|---|---|
| Soil pat diameter | 45 mm |
| Soil pat height | 15 mm |
| Mercury unit weight | 13.6 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
IS 2720 Part 6: Calculation of Shrinkage Factors
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:
Specific Gravity, G: Determined as per IS 2720 Part 3.
| Parameter | Symbol | Unit/Description | Reference Clause |
|---|---|---|---|
| Shrinkage Limit | ( w_s ) | % water content where shrinkage stops | 7.4 |
| Shrinkage Ratio | ( R ) | Volume change per unit water content change | 2.1.4 |
| Volumetric Shrinkage | ( V_3 ) | % volume change due to drying | 7.5 |
| Specific Gravity | ( G ) | Unitless, soil solids density ratio | IS 2720 Part 3 |
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
IS 2720 Part 6: Reporting of Results - Key Points
Test Repetition & Averaging (Clause 8.2):
Rounding Off (Clause 0.5):
Record Format (Clause 8.1):
[ w = \frac{W_w}{W_s} \times 100 ]
Where:
| Step | Requirement |
|---|---|
| Number of Tests | Minimum 3 per sample |
| Acceptable Variation | ± 2% from average |
| Rounding | As per IS 2-1960 |
| Documentation Format | Appendix 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.
IS 2720 Part 6: Pro Forma for Record of Test Results (Appendix A)
Test Reporting Requirements (Clause 8.1 & 8.2):
Pro Forma Elements (Appendix A) typically include:
Key Formula for Dry Density (Clause 5.4 reference):
[ \text{Dry Density} (\rho_d) = \frac{\text{Bulk Density} (\rho)}{1 + w} ]
Where:
| Parameter | Details/Units | Remarks |
|---|---|---|
| Sample ID | Text | Location, depth, date |
| Bulk Density ((\rho)) | g/cm³ or kN/m³ | Measured |
| Water Content (w) | % or decimal | Measured |
| Dry Density ((\rho_d)) | g/cm³ or kN/m³ | Calculated |
| Individual Test Values | Numeric | At least 3 readings |
| Average Value | Numeric | Mean of valid test results |
| Observations/Remarks | Text | Deviations, 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 (
Frequently Asked
According to IS 2720 Part 6, the apparatus required for determining the shrinkage limit includes:
This mercury displacement method is essential to determine the volume of the dry soil pat accurately.
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This setup ensures precise volume measurement critical for shrinkage limit determination.
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).
Sample State:
Volume Change Behavior:
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Summary:
Shrinkage limit depends on soil structure; undisturbed soil reflects in-situ conditions, remoulded soil reflects disturbed conditions with typically higher shrinkage limits.
Procedure for Measuring Volumetric Shrinkage Using Mercury Displacement (IS 2720 Part 6):
Prepare Soil Pat:
Measure Volume of Oven-Dry Soil Pat (V'o):
Measure Volume of Wet Soil Pat (V):
Volumetric Shrinkage Calculation: [ \text{Volumetric Shrinkage} = \frac{V - V'_o}{V} \times 100% ]
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For accurate shrinkage limit testing per IS 2720 Part 6, follow these key steps for soil sample preparation and handling:
| Step | Dimension / Quantity | Notes |
|---|---|---|
| Soil pat size (undisturbed) | 45 mm dia × 15 mm height | Rounded edges |
| Soil sample (remoulded) | ~100 g, passing 425-micron sieve | Thoroughly mixed |
| Shrinkage dish filling | ~1/3 volume increments | Tap to remove air, grease inside |
| Mercury displacement | Weight to 0.1 g accuracy | Avoid air entrapment |
This ensures precise volume measurement critical for shrinkage limit determination.
IS 2720 Part 6: Shrinkage Ratio and Volumetric Shrinkage
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:
Alternatively, expressed as a percentage of dry volume change per % water content change.
Calculated using:
[ V_3 = (w_1 - w_s) \times R ]
Where:
| Parameter | Symbol | Unit/Dimension | Description |
|---|---|---|---|
| Shrinkage Ratio | R | Dimensionless | Volume change per unit water loss |
| Volumetric Shrinkage | V₃ | Percentage of volume | Total volumetric shrinkage |
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This provides a clear method to quantify soil volume changes due to drying beyond the shrinkage limit.
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