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IS 2720 Part 11 : 1986Methods of test for soils - Determination of shear strength parameters of a soil by consolidated undrained triaxial compression test with pore water pressure measurement

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CurrentSpecializedTesting MethodGeotechnical · Soil and Foundation
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IS 2720:1986 Part 11 is the Indian Standard (BIS) for methods of test for soils - determination of shear strength parameters of a soil by consolidated undrained triaxial compression test with pore water pressure measurement. This standard outlines the procedure for conducting a consolidated undrained (CU) triaxial compression test with pore water pressure measurement on soil. It determines the effective shear strength parameters (effective cohesion and effective angle of internal friction) necessary for advanced geotechnical stability analyses.

Describes the procedure for conducting consolidated undrained triaxial compression tests with pore water pressure measurement to determine soil shear strength parameters.

Overview

Status
Current
Usage level
Specialized
Domain
Geotechnical — Soil and Foundation
Type
Testing Method
Also on InfraLens for IS 2720
4Key values1Handbook topics3Knowledge articles3FAQs
Practical Notes
! Ensure complete saturation of the specimen and de-airing of the pore pressure measuring lines before starting the test, typically verified by a B-value of 0.95 or higher.
! The rate of strain during shearing must be slow enough to allow equalization of pore water pressure throughout the specimen; this is critical in clayey soils.
! Filter paper drains can be used to accelerate the consolidation and saturation phases for highly impermeable soils.
Frequently referenced clauses
Cl. 3Preparation of Test SpecimensCl. 4.2Saturation of SpecimenCl. 4.3ConsolidationCl. 4.4Shearing (Measurement of pore pressure)Cl. 5Calculations
Pulled from IS 2720:1986. Browse the full clause & table index below in Tables & Referenced Sections.
soilcohesive soilsandclay

International Equivalents

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Key Values4

Quick Reference Values
length to diameter ratio2 to 2.5
minimum specimen diameter38 mm
maximum particle sizeOne-sixth of the specimen diameter
acceptable B value for saturation>= 0.95
Key Formulas
sigma_1' = sigma_1 - u (Effective major principal stress)
sigma_3' = sigma_3 - u (Effective minor principal stress)
B = Delta u / Delta sigma_3 (Pore pressure parameter B)
A = Delta u / (Delta sigma_1 - Delta sigma_3) (Pore pressure parameter A)

Tables & Referenced Sections

Key Tables
No tables data
Key Clauses
Clause 3 - Preparation of Test Specimens
Clause 4.2 - Saturation of Specimen
Clause 4.3 - Consolidation
Clause 4.4 - Shearing (Measurement of pore pressure)
Clause 5 - Calculations

Related Resources on InfraLens

Handbook & Design Rules
Handbook Topics
📖Earthwork Bulking & Shrinkage Factors
→
Articles & Guides
📖IS 2720 Soil Testing — All Parts Complete Guide
→
📖Soil Bearing Capacity per IS 1904
→
📖Foundation Selection Guide
→

Frequently Asked Questions3

What is the standard specimen size for the triaxial test?+
The minimum diameter is 38 mm, and the length-to-diameter ratio should be between 2.0 and 2.5.
How do you verify if the soil sample is fully saturated?+
By conducting a B-value check. A B-value (ratio of change in pore pressure to change in cell pressure) of 0.95 or greater generally indicates full saturation.
Why is the test performed at a very slow strain rate?+
To ensure uniform distribution and accurate measurement of pore water pressure within the specimen without inducing localized pressure gradients.

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