IS 2720 Part 351974AI Search Enabled✦ AI Generated

Methods of test for soils, Part 35: Measurement of negative pore water pressure

IS 2720 Part 35 (1974) specifies the method for measuring negative pore water pressure in partially saturated soils, a critical parameter influencing soil strength and stability. It details both direct measurement techniques for pressures up to -0.75 kg/cm² and indirect measurement using the axis translation technique for greater negative pressures. This standard is essential for geotechnical engineers and soil testing laboratories involved in soil mechanics and foundation engineering.

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135Clauses Indexed
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1974Edition
Soil and Foundation EngineeringCategory
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What This Standard Covers

IS 2720 Part 35 (1974) specifies the method for measuring negative pore water pressure in partially saturated soils, a critical parameter influencing soil strength and stability. It details both direct measurement techniques for pressures up to -0.75 kg/cm² and indirect measurement using the axis translation technique for greater negative pressures. This standard is essential for geotechnical engineers and soil testing laboratories involved in soil mechanics and foundation engineering.

Who Uses This Standard

  • Geotechnical Engineers
  • Soil Testing Laboratory Technicians
  • Foundation Design Engineers
  • Civil Engineers specializing in Soil Mechanics
  • Research Scientists in Soil Physics
  • Construction Quality Control Engineers
  • Academic Researchers in Geotechnical Engineering

Key Topics Covered

Negative pore water pressure in partially saturated soils
Direct measurement techniques for negative pore water pressure
Axis translation technique for indirect measurement
Use and calibration of fine ceramic porous stones
Saturation and de-airing of pore water pressure lines
Apparatus setup including mercury manometers and pressure gauges
Preparation and sealing of soil samples
Air entry value determination of ceramic stones
Pressure control and equilibrium procedures
Leak detection and system maintenance
Data recording and interpretation
Safety and handling of mercury and compressed air systems

Table of Contents

1Scope

IS 2720 Part 35 (1974) - Scope & Key Specifications

This part covers methods for preparation and testing of soil specimens, including accessories and apparatus used.

Key Points from Scope & Clauses:

  • Clause 2.1: Terminology follows IS 2809-1972 (Glossary of soil engineering terms).

  • Clause 3.4.6: Seamless Rubber Membrane

    • Used for specimen extrusion.
    • Tube open at both ends.
    • Internal diameter = specimen diameter.
    • Length = specimen height + 50 mm.
    • Thickness: 0.2 to 0.3 mm (depends on soil strength and size).
  • Clause 3.4.20: Accessories

    • Includes tools for specimen preparation, extrusion, trimming.
    • Measurement tools for size, weight, water content.

Typical Dimensions for Rubber Membrane

ParameterValue
Internal DiameterEqual to specimen diameter
LengthSpecimen height + 50 mm
Thickness0.2 to 0.3 mm

Summary Diagram: Specimen with Rubber Membrane

flowchart LR
    A[Soil Specimen] -->|Encased by| B[Seamless Rubber Membrane]
    B -->|Length = Specimen height + 50 mm| C[Membrane Length]
    B -->|Diameter = Specimen diameter| D[Membrane Diameter]
    B -->|Thickness 0.2-0.3 mm| E[Membrane Thickness]

This standard ensures consistent specimen preparation for reliable soil testing results. For detailed procedures, refer to full IS 2720 Part 35 text.

3Apparatus

IS 2720 Part 35: Apparatus Specifications

Apparatus Components (Clause 3.4)

  • The apparatus typically includes:
    • A loading frame
    • A dial gauge or displacement measuring device
    • A container for soil sample
    • Plates or porous stones for drainage
    • Water supply system for saturation and consolidation
    • Pressure gauge for measuring pore water pressure

Preparation (Clauses 6.1 & 7.1)

  • Apparatus should be prepared as per Fig. 1 (refer IS 2720-35 for detailed schematic).
  • Ensure all components are clean, calibrated, and assembled correctly.
  • Follow the dimensions and setup as indicated in Clauses 3.2 and 3.3.

Environmental Conditions (Clause 3.6)

  • Maintain constant ambient temperature during measurements to ensure accuracy.

Key Notes:

ParameterSpecification/Requirement
Ambient TemperatureKeep constant during testing
Displacement MeasurementUse dial gauge with 0.01 mm accuracy
Pressure MeasurementUse calibrated pressure gauges
Sample Container DimensionsAs per Fig. 1 (typically 60 mm dia)

flowchart LR
    A[Soil Sample] --> B[Porous Stone]
    B --> C[Loading Plate]
    C --> D[Loading Frame]
    D --> E[Dial Gauge]
    F[Water Supply] --> G[Sample Container]
    G --> B
    H[Pressure Gauge] --> G

For exact dimensions and detailed apparatus setup, refer to Fig. 1 of IS 2720 Part 35.

4Saturation of Fine Ceramic Porous Stone and De-airing of Pore Water Pressure Lines

IS 2720 Part 35: Saturation & De-airing of Fine Ceramic Porous Stone and Pore Water Pressure Lines

Key Points from the Code:

  • Ceramic Porous Stone:

    • Diameter = 32 mm
    • Thickness = 10 mm
    • Air entry value > maximum negative pore water pressure to be measured (Clause 3.4.7)
  • Saturation & De-airing (Clause 4.2):

    • Essential for measuring negative pore water pressure.
    • Use de-aired water to saturate the ceramic stone and pore pressure lines.
    • All valves start closed to avoid air entry.
    • Thorough removal of air from lines is critical to avoid measurement errors.

Procedure Summary:

  1. Connect the apparatus with valves closed.
  2. Fill pore pressure lines and ceramic stone with de-aired water (water boiled and cooled in a vacuum to remove dissolved gases).
  3. Open valves gradually to allow water to saturate the stone and displace air.
  4. Repeat de-airing until no air bubbles appear in the lines.

Important Specification:

ParameterValue
Ceramic stone diameter32 mm
Ceramic stone thickness10 mm
Air entry value> max negative pore pressure

Conceptual Mermaid Diagram:

flowchart LR
    A[De-aired Water Reservoir] --> B[Valve Closed]
    B --> C[Fine Ceramic Porous Stone (32 mm x 10 mm)]
    C --> D[Pore Water Pressure Line]
    D --> E[Pressure Transducer]
    style B fill:#f9f,stroke:#333,stroke-width:2px
    style C fill:#bbf,stroke:#333,stroke-width:2px

Summary: Saturate the ceramic stone and pore lines with de-aired water under closed valve conditions to ensure accurate negative pore water pressure measurement.

5Soil Sample for Test

IS 2720 Part 35 (1974) - Soil Sample for Test: Key Points

Accessories (Clause 3.4.20)

  • Includes tools for extrusion, trimming, size & weight measurement, water content determination.
  • Essential for preparing undisturbed soil specimens.

Saturation & Air Entry Value (Clause 4.3.6)

  • Ceramic stones used for measuring negative pore water pressure must be saturated and de-aired before use.
  • Air entry value of ceramic stone is measured once to define its effective pressure range.

Application of Pressure (Clause 7.9)

  • Valves A1 and A2 are opened; pore air pressure applied via A1, cell pressure via C1.
  • Both pressures should be equal and increased in 0.5 kg/cm² increments.
  • In soils with continuous air phase, equal increments in cell and pore air pressure cause corresponding increases in pore water pressure.

Summary Table: Pressure Application

ParameterValvePressure ApplicationIncrement Step
Pore Air PressureA1Applied to soil sample0.5 kg/cm²
Cell PressureC1Applied simultaneously0.5 kg/cm²

Practical Notes:

  • Ensure saturation and de-airing of ceramic stones before testing.
  • Maintain equal magnitude of cell and pore air pressures to simulate in-situ conditions.
  • Use accessories for accurate specimen preparation and measurement.
flowchart LR
    A[Start: Soil Sample Preparation]
    B[Use Accessories: Extrusion, Trimming, Measurement]
    C[Saturate & De-air Ceramic Stone]
    D[Open Valves A1 & A2]
    E[Apply Pore Air Pressure (A1)]
    F[Apply Cell Pressure (C1)]
    G[Increase Pressures in 0.5 kg/cm² Steps]
    H[Measure Pore Water Pressure]
    A --> B --> C --> D --> E & F --> G --> H

This ensures reliable soil testing per IS 2720 Part 35.

6Procedure for Direct Measurement of Negative Pore Water Pressure

IS 2720 Part 35: Procedure for Direct Measurement of Negative Pore Water Pressure


Key Points from Clause 5.1 & Procedure Overview

  • Sample Preparation:

    • Diameter of soil sample = Diameter of triaxial cell pedestal.
    • Sample height: Any convenient height is acceptable.
    • Applicable for field samples or lab-prepared samples (compacted, remoulded, etc.).
  • Measurement Principle:

    • Negative pore water pressure (matric suction) is measured directly using specialized equipment (e.g., tensiometers) embedded in the soil sample.
    • The device measures the tension in pore water, indicating suction.

Typical Measurement Setup

flowchart LR
    A[Soil Sample] --> B[Trimmed to pedestal diameter]
    B --> C[Placed in Triaxial Cell]
    C --> D[Tensiometer inserted]
    D --> E[Direct measurement of negative pore water pressure]

Important Considerations

  • Ensure good contact between tensiometer and soil for accurate readings.
  • Maintain saturation of tensiometer porous tip.
  • Readings typically range from 0 to -100 kPa (limited by tensiometer range).
  • For higher suctions, other methods (e.g., filter paper) are used.

Formula (Conceptual)

[ u = -\sigma_w ]

Where:

  • ( u ) = Negative pore water pressure (suction) [kPa]
  • ( \sigma_w ) = Water tension measured by tensiometer [kPa]

Summary Table: Sample Dimensions

ParameterSpecification
Sample DiameterEqual to triaxial cell pedestal diameter
Sample HeightAny convenient height
Measurement Range0 to -100 kPa (typical tensiometer)

For detailed calibration and apparatus specifications, refer to the full IS 2720 Part 35 document.

7Procedure for Indirect Measurement of Negative Pore Water Pressure Using the Axis-Translation Technique

IS 2720 (Part 35) - Axis-Translation Technique for Negative Pore Water Pressure

Key Specifications & Setup

  • Sample Preparation: Diameter equal to triaxial cell pedestal; height flexible.
  • Apparatus: As per Fig. 1 (IS 2720 Part 35), same for direct & indirect measurements.
  • Valves: Open B1, D2; close D1, D2, D3, Da, D5 after sample assembly.
  • De-airing: Essential if air outgassing occurs (Clause 4.2).

Procedure Summary (Clause 6.11)

  1. Open valves B1 and D2.
  2. Disassemble soil sample.
  3. Reduce pressure in X to zero.
  4. Close valves D1, D2, D3, Da, D5.
  5. Allow water flow from burette to ceramic stone top.
  6. Clean ceramic stone top.
  7. Ready for next measurement or de-air if required.

Axis-Translation Principle

  • Increase air pressure above atmospheric in the chamber.
  • Keep pore water pressure at atmospheric or lower.
  • Measure negative pore water pressure indirectly by controlling air pressure and measuring water pressure.

Formula for Negative Pore Water Pressure (u)

[ u = P_a - P_w ] Where:

  • (P_a) = Applied air pressure (above atmospheric)
  • (P_w) = Measured pore water pressure

Diagram: Simplified Axis-Translation Setup

flowchart LR
    A[Air Pressure Chamber] -->|Pressurizes air| B[Soil Sample]
    B -->|Pore water pressure| C[Ceramic Stone]
    C -->|Water flow| D[Burette]
    D -->|Measurement| E[Pressure Gauge]

Note: Accurate sealing and de-airing are critical to avoid errors in negative pore water pressure measurement.

Popular Questions About IS 2720 Part 35

?What is the axis translation technique and how is it applied in this standard?

Axis Translation Technique (IS 2720 Part 35)

The axis translation technique is an indirect method to measure negative pore water pressure (matric suction) in partially saturated soils.

Key Points:

  • Purpose: To measure negative pore water pressures beyond the direct measurement range (0 to -0.75 kg/cm²).
  • Principle: Increase the pore air pressure artificially, shifting the pore water pressure to a positive range where it can be measured.
  • Limitation: The maximum measurable suction is limited by the air entry value of the fine ceramic porous stone used.
  • Setup: The apparatus (Fig. 1 in the standard) allows both direct and axis translation measurements.
  • Procedure:
    • Increase pore air pressure while maintaining water pressure measurement.
    • Ensure no air bubbles are in the pore water line (de-airing as per clause 4.2).
    • Control valves as per clause 6.11 for sample preparation and measurement.

Summary in steps:

  1. Apply increased pore air pressure (positive).
  2. Pore water pressure shifts above zero.
  3. Measure pore water pressure indirectly.
  4. Correct for applied air pressure to find negative pore water pressure.
Loading diagram...

This technique enables accurate measurement of matric suction in soils where direct measurement is not feasible.

?How is the fine ceramic porous stone prepared and calibrated for testing?

Preparation and Calibration of Fine Ceramic Porous Stone (IS 2720 Part 35)

  • Dimensions: Ceramic stone of 32 mm diameter and 10 mm thickness.
  • Air Entry Value: Must exceed the absolute negative pore water pressure to be measured.
  • Saturation & De-airing: Before testing, saturate and de-air the stone and connected pore water lines to avoid air intrusion (Clause 4.3.6).
  • Calibration Procedure (Clause 4.3.4):
    • Apply air pressure in increments of 0.5 kg/cm² initially.
    • As pressure nears expected air entry value, reduce increments to 0.1 kg/cm².
    • Maintain each pressure increment for 30 minutes.
    • Record water level in burette before increasing pressure.
  • Purpose: Calibration determines the air entry value once, defining the stone's usable range.
Loading diagram...

This ensures accurate measurement of negative pore water pressure in soil testing.

?What apparatus is required for measuring negative pore water pressure according to IS 2720 Part 35?

According to IS 2720 Part 35, the apparatus required for measuring negative pore water pressure (also called soil suction) typically includes:

  • Tensiometer: The primary instrument used, which consists of:

    • A porous ceramic cup (saturated with water) in contact with soil.
    • A water reservoir connected to a pressure gauge.
    • A pressure gauge or manometer to measure the tension (negative pressure) developed in the water.
  • Pressure gauge/manometer: To read the negative pressure (suction) in units like kPa or cm of water.

  • Saturation setup: To ensure the porous cup is fully saturated before insertion.

Working principle: The tensiometer equilibrates water pressure between soil and the water in the device. Negative pore water pressure in soil creates tension, which is measured by the gauge.


Summary:

ApparatusPurpose
Porous ceramic cupSoil-water interface
Water reservoirTransmits pressure
Pressure gaugeMeasures negative pore water pressure

This setup is standard for measuring soil suction as per IS 2720 Part 35.

?How does the standard ensure accuracy and prevent leaks during measurement?

IS 2720 Part 35 ensures accuracy and prevents leaks during pore water pressure measurement through these key provisions:

  • Leak Prevention (Clause 7.3): All valves, connections, and joints must be checked meticulously to ensure no leaks exist, which could compromise pressure readings.

  • Stable Environment (Clause 3.6): Measurements should be conducted where ambient temperature is kept constant to avoid volume/pressure fluctuations.

  • Balancing Manometer Setup (Clause 3.5):

    • Maintains positive pressure in most of the system, minimizing cavitation risk in the negative pressure zone.
    • Minimizes water volume under negative pressure by placing valve B1, null indicator, and balancing manometer as close to the cell as possible.
    • Thorough deaeration of water in this zone is mandatory to prevent air bubbles affecting readings.
  • Mercury Level Control (Clause 6.5): Proper valve operation and mercury level marking ensure a stable null reference, with water maintained above the ceramic stone to maintain hydraulic continuity.

Loading diagram...

Summary: Leak-tight valves, minimal negative pressure volume, deaerated water, and stable mercury levels collectively ensure accurate, leak-free pore water pressure measurement.

?What are the limitations on the range of negative pore water pressure that can be measured?

Limitations on the range of negative pore water pressure measurement (IS 2720 Part 35):

  • Negative pore water pressure (tension) exists due to surface tension at air-water interfaces in partially saturated soils.

  • Measurement is delicate because water under tension is prone to cavitation (formation of vapor cavities), which limits the measurable negative pressure range.

  • The volume of water subjected to negative pressure in the measurement system must be minimized to reduce cavitation risk.

  • Proper system setup requires:

    • Locating valves and null indicator as close to the soil sample as possible.
    • Using a balancing manometer to maintain positive pressure in most of the system.
    • Thoroughly deaerating water to avoid cavitation nuclei.
  • The maximum negative pore water pressure measurable is limited by the cavitation threshold of water, typically around -100 to -150 kPa under laboratory conditions.

  • The method measures negative pore water pressure indirectly as:

    [ |u_w| = p_a - u_w^{+} ]

    where:
    ( |u_w| ) = absolute negative pore water pressure,
    ( p_a ) = applied pore air pressure,
    ( u_w^{+} ) = measured positive pore water pressure at equilibrium.


Summary Table

ParameterDetail
Max negative pore water pressure~ -100 to -150 kPa (limited by cavitation)
Key limitationCavitation in water column
System designMinimize water volume, deaerate water, locate valves close to sample
Measurement principleNegative pressure = air pressure - positive water pressure
Loading diagram...

This setup confines tension to a minimal water volume to avoid cavitation and ensures reliable measurement.

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