IS 2720 Part 10:1991 specifies the standardized procedure for determining the unconfined compressive strength of clayey soils, including undisturbed, remoulded, or compacted specimens. This test measures the soil's compressive and shearing strength in an undrained state by applying axial strain until failure, providing critical data for geotechnical design and analysis. It is essential for engineers assessing soil stability and strength characteristics under load.
Overview
IS 2720 Part 10:1991 specifies the standardized procedure for determining the unconfined compressive strength of clayey soils, including undisturbed, remoulded, or compacted specimens. This test measures the soil's compressive and shearing strength in an undrained state by applying axial strain until failure, providing critical data for geotechnical design and analysis. It is essential for engineers assessing soil stability and strength characteristics under load.
Audience
Contents
Structure
IS 2720 Part 10: Scope & Key Specifications
This part of IS 2720 covers the Determination of Unconfined Compressive Strength of soil specimens.
| Parameter | Symbol | Unit |
|---|---|---|
| Initial Diameter | Do | mm |
| Initial Length | Lo | mm |
| Initial Cross-sectional Area | Ao | cm² |
| Initial Volume | V | cm³ |
| Initial Mass | - | g |
| Initial Density | ρ | g/cm³ or kg/m³ |
| Initial Water Content | w | % |
| Initial Degree of Saturation | Sr | % |
| Specific Gravity of Soil | G | - |
Axial Strain (e): [ e = \frac{\Delta L}{L_0} = \frac{L - L_0}{L_0} ]
Cross-sectional Area under deformation (A): [ A = A_0 (1 - e) ]
Compressive Stress (σ): [ \sigma = \frac{P}{A} \quad \text{where } P = \text{axial force (N or kgf)}, A = \text{area (cm}^2) ]
Unconfined Compressive Strength (qu): [ q_u = \text{Maximum compressive stress at failure (kPa)} ]
Undrained Shear Strength (su) (if applicable): [ s_u = \frac{q_u}{2} ]
| Deformation Dial Reading (mm) | Axial Strain (e) | Area (cm²) | Proving Ring Reading | Axial Force (N) | Compressive Stress (kPa) | Remarks | |-------------------------------|------------------|------------|---------------------|-----------------|
IS 2720 Part 10 references several key standards and provides essential test data formats and specimen details for unconfined compression tests on soils.
| Parameter | Symbol | Unit | Notes |
|---|---|---|---|
| Initial diameter | Do | mm | Measured before test |
| Initial length | Lo | mm | Measured before test |
| Initial area | Ao | cm² | ( Ao = \pi \times (Do/2)^2 ) |
| Axial deformation | ΔL | mm | Dial gauge reading |
| Axial strain | ( e = \frac{\Delta L}{L_o} ) | - | Ratio of deformation to initial length |
| Area during test | ( A = A_o (1 - e) ) | cm² | Assuming volume constancy |
| Axial force | P | N (kgf) | Measured by proving ring |
| Compressive stress | ( \sigma = \frac{P}{A} ) | kPa (kg/cm²) | Stress on specimen |
flowchart TD
A[Initial Specimen] --> B[Measure Do, Lo]
B --> C[Calculate Ao = π(Do/2)^2]
C --> D[Apply axial load P]
D --> E[Measure deformation ΔL]
E --> F[Calculate strain e = ΔL/Lo]
F --> G[Calculate current area A = Ao(1 - e)]
G --> H[Calculate stress σ = P/A]
H --> I[Determine qu, undrained shear strength]
Note: Always ensure use of latest revisions and amendments from BIS for compliance and accuracy.
IS 2720 Part 10: Definitions & Key Formulas (SI Units)
| Parameter | Formula/Description |
|---|---|
| Axial deformation ( \Delta L ) | Dial reading (mm) |
| Axial strain ( e ) | ( e = \frac{\Delta L}{L_0} ) |
| Area at strain ( A ) | ( A = A_0 (1 - e) ) (cm²) |
| Axial force ( F ) | From proving ring dial reading (N or kgf) |
| Compressive stress ( \sigma ) | ( \sigma = \frac{F}{A} ) (kPa or kg/cm²) |
[ \text{Axial strain}, e = \frac{\Delta L}{L_0} ] [ \text{Area at strain}, A = A_0 (1 - e) ] [ \text{Compressive stress}, \sigma = \frac{F}{A} ]
IS 2720 Part 10: Apparatus & Key Parameters for Unconfined Compression Test
| Parameter | Formula/Notes |
|---|---|
| Axial deformation, ( \Delta L ) (mm) | From dial gauge readings |
| Axial strain, ( e = \frac{\Delta L}{L_0} ) | Dimensionless strain |
| Area during test, ( A = A_0 (1 - e) ) | Adjusted for deformation |
| Axial force, ( F ) (N or kgf) | From proving ring dial reading × calibration factor |
| Compressive stress, ( \sigma = \frac{F}{A} ) (kPa) | Stress on specimen cross-section |
Axial strain: e = ΔL / L₀
Area during test: A = A₀ (1 - e)
Compressive stress: σ = F / A
flowchart TD
A[Initial Specimen] --> B[Measure D₀, L₀, A₀]
B --> C[Apply Load]
C --> D[Record Dial Gauge ΔL]
D -->
IS 2720 Part 10: Preparation of Test Specimen - Key Points
| Parameter | Symbol | Unit |
|---|---|---|
| Initial Diameter | D₀ | mm |
| Initial Length (Height) | L₀ | mm |
| Initial Cross-sectional Area | A₀ | cm² |
| Initial Volume | V₀ | cm³ |
| Initial Mass | m₀ | g |
| Initial Density | ρ₀ | g/cm³ or kg/m³ |
| Initial Water Content | w₀ | % |
| Initial Degree of Saturation | S₀ | % |
| Observation | Symbol/Formula |
|---|---|
| Axial Deformation | ΔL (mm) |
| Axial Strain | ( e = \frac{\Delta L}{L_0} ) |
| Area during test | ( A = A_0 (1 - e) ) |
| Compressive Stress | ( \sigma = \frac{P}{A} ) (kPa) |
| Proving Ring Reading | Dial reading (N or kgf) |
[ e = \frac{\Delta L}{L_0} ]
[ A = A_0 (1 - e) ]
[ \sigma = \frac{
IS 2720 Part 10 - Test Procedure Key Points
| Parameter | Formula/Note |
|---|---|
| Axial deformation, (\Delta L) | Measured from dial gauge (mm) |
| Axial strain, (e = \frac{\Delta L}{L_0}) | Dimensionless |
| Area during test, (A = A_0 (1 - e)) | Accounts for specimen shortening |
| Compressive force, (P) (N or kgf) | From proving ring dial reading |
| Compressive stress, (\sigma = \frac{P}{A}) (kPa or kg/cm²) | Stress on specimen cross-section |
flowchart TD
A[Prepare Specimen] --> B[Measure Initial Dimensions]
B --> C[Apply Axial Load]
C --> D[Record Dial Reading & Load]
D --> E[Calculate Strain & Stress]
E --> F[Determine \(q_u\) and \(s_u\)]
F --> G[Analyze Failure & Water Content]
``
IS 2720 Part 10: Calculations and Plotting for Unconfined Compression Test
| Parameter | Symbol | Formula / Notes |
|---|---|---|
| Initial diameter | ( D_0 ) mm | Measured before test |
| Initial length | ( L_0 ) mm | Measured before test |
| Initial area | ( A_0 ) cm² | ( A_0 = \pi (D_0/2)^2 ) |
| Axial deformation | ( \Delta L ) mm | From dial reading |
| Axial strain | ( e = \frac{\Delta L}{L_0} ) | Dimensionless |
| Area during test | ( A = A_0 (1 - e) ) | Assuming volume constancy |
| Axial force | ( P ) N or kgf | From proving ring dial reading |
| Compressive stress | ( \sigma = \frac{P}{A} ) KPa or kg/cm² | Stress on specimen cross-section |
| Unconfined compressive strength | ( q_u ) KPa | Maximum compressive stress before failure |
| Undrained shear strength | ( s_u = \frac{q_u}{2} ) KPa (if applicable) | For cohesive soils |
| Deformation (mm) | Axial Strain (e) | Area (A) (cm²) | Dial Reading | Axial Force (P) (N) | Stress (\sigma) (KPa) | Remarks |
|---|---|---|---|---|---|---|
graph TD
A[Initial Specimen] --> B[Measure \(D_0, L_0\)]
B --> C[Calculate \(
IS 2720 Part 10: Recording of Observations for Unconfined Compression Test
Soil Sample Details:
Apparatus Details:
Soil Specimen Details:
Compression Test Observations:
| Parameter | Description |
|---|---|
| Rate of strain | Controlled deformation rate |
| Deformation dial reading (mm) | Axial deformation (ΔL) |
| Axial strain (e) | ( e = \frac{\Delta L}{L_0} ) |
| Area (A) | ( A = A_0 (1 - e) ) (assuming volume constancy) |
| Proving ring dial reading | Load measurement |
| Axial force (N or kgf) | Calculated from dial reading and calibration |
| Compressive stress (qu) | ( q_u = \frac{\text{Axial force}}{A} ) (KPa) |
| Remarks | Observations on failure, particle size, etc. |
[ \text{Axial strain}, e = \frac{\Delta L}{L_0} ]
[ \text{Area at any time}, A = A_0 (1 - e) ]
[ \text{Compressive stress}, q_u = \frac{P}{A} \quad \text{where } P = \text{axial load
IS 2720 (Part 10) - Pro Forma for Record of Observations:
The pro forma (Annex A) for unconfined compression test records the following:
| Deformation Dial Reading | Axial Deformation (mm) | Axial Strain, ( e = \frac{\Delta L}{L_0} ) | Area ( A = A_0 (1 - e) ) (cm²) | Proving Ring Dial Reading | Axial Force (N) | Compressive Stress ( \sigma = \frac{Force}{Area} ) (kPa) | Remarks |
|---|
Initial Area: [ A_0 = \pi \left(\frac{D_0}{2}\right)^2 ]
Axial Strain: [ e = \frac{\Delta L}{L_0} ]
Area during test: [ A = A_0 (1 - e) ]
Compressive Stress: [ \sigma = \frac{Force}{Area} ]
Unconfined Compressive Strength: [ q
Frequently Asked
According to IS 2720 Part 10 (1991), the unconfined compressive strength (UCS) test is applicable primarily to clayey soils. Key points on suitable soil specimens:
Types of specimens:
Restrictions:
Purpose:
| Soil Type | Specimen Type | Suitability for UCS Test |
|---|---|---|
| Clayey soils | Undisturbed, remoulded, compacted | Suitable |
| Silty or sandy soils | Any | Not suitable |
This ensures reliable UCS values for clayey soils under undrained conditions.
IS 2720 Part 10: Specimen Dimensions and Size Limitations
Summary Table:
| Parameter | Value/Range |
|---|---|
| Diameter (D) | ≥ 38 mm |
| Max particle size | < D/8 (e.g., < 4.75 mm) |
| Height (H) | H = 2D to 2.5D |
| Cross-section | Circular, uniform |
| End faces | Perpendicular to axis |
| Measurement precision | ± 0.1 mm |
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This ensures reliable and standardized test results per IS 2720 Part 10.
IS 2720 Part 10 Apparatus & Measurement Devices Summary:
Compression Device (Clause 4.1):
Must have adequate capacity and strain control. Types include:
Vernier Callipers (Clause 4.4):
For measuring specimen dimensions accurately to 0.1 mm.
Timing Device (Clause 4.5):
To record elapsed test time with 1-second accuracy, essential for strain rate control.
| Apparatus | Purpose | Accuracy/Capacity |
|---|---|---|
| Compression Device | Apply controlled load | Sufficient capacity & strain control |
| Vernier Callipers | Measure specimen dimensions | ±0.1 mm |
| Timing Device | Measure elapsed time | ±1 second |
This ensures precise load application, dimension measurement, and timing for reliable test results.
According to IS 2720 Part 10, the unconfined compressive strength (qu) is determined as follows:
Calculate axial strain:
[
\varepsilon = \frac{\Delta L}{L_0}
]
where ( \Delta L ) = axial deformation, ( L_0 ) = initial length.
Calculate instantaneous cross-sectional area:
[
A = A_0 (1 - \varepsilon)
]
assuming volume constancy.
Calculate compressive stress:
[
\sigma = \frac{P}{A}
]
where ( P ) = axial load.
Plot ( \sigma ) vs. ( \varepsilon ) and find maximum ( \sigma ) or stress at 20% strain.
| Parameter | Symbol | Unit |
|---|---|---|
| Initial length | (L_0) | mm |
| Axial deformation | (\Delta L) | mm |
| Axial strain | (\varepsilon) | (dimensionless) |
| Initial area | (A_0) | cm² |
| Cross-sectional area | (A) | cm² |
| Load | (P) | N or kgf |
| Compressive stress | (\sigma) | kPa or kg/cm² |
| Unconfined compressive strength | (q_u) | kPa or kg/cm² |
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According to IS 2720 Part 10 (1991), Clause 5.1 and the Note, the unconfined compression test is NOT suitable for soils containing appreciable quantities of sand or silt. This is because:
For sandy or silty soils, consider triaxial shear tests or direct shear tests that apply lateral confinement and better simulate in-situ conditions.
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Key takeaway: IS 2720 Part 10 unconfined compression test is for cohesive soils only, not sandy or silty soils.
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