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Method of test for determination of water transmission rate by capillary action through natural building stones
1967 Edition

This standard outlines a laboratory procedure for measuring the rate at which water travels through natural building stones by capillary action. It is crucial for evaluating dense natural stones for their effectiveness in waterproofing and damp-proofing construction applications. The document specifies specimen preparation, testing setup, environmental conditions, and data analysis to guarantee uniform assessment of water transmission characteristics.

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What This Standard Covers

This standard outlines a laboratory procedure for measuring the rate at which water travels through natural building stones by capillary action. It is crucial for evaluating dense natural stones for their effectiveness in waterproofing and damp-proofing construction applications. The document specifies specimen preparation, testing setup, environmental conditions, and data analysis to guarantee uniform assessment of water transmission characteristics.

Who Uses This Standard

  • Structural Engineers
  • Material Testing Facilities
  • Construction Quality Assurance Professionals
  • Geotechnical Specialists
  • Stone Quarry Supervisors
  • Research Scientists in Building Materials
  • Waterproofing Consultants

Key Topics Covered

Preparation and sizing of test specimens
Configuration of testing equipment
Methods for sealing to prevent leaks
Controlled environmental testing conditions
Procedures for measuring water transmission
Recording and timing of specimen weighing
Calculations for water loss via capillary action
Guidelines for result documentation and analysis
Sampling strategies for quarry and field stones
Application of paraffin wax and resin sealing
Standardization of test environment
Correlation to waterproofing efficiency

Table of Contents

1Scope and Application

Overview of the Standard and Essential Specifications

  • Scope: Defines the method to quantify water transmission rate through stones by capillary action, relevant for waterproofing uses.
  • Measurement Units: Water loss expressed in grams over a 48-hour period after stabilization (Clause 6.3).
  • Balance Accuracy: Requires precision of 0.01 g for weighing (Clause 4.3).
  • Test Assembly: Comprises waterproofing compound, distilled water, and a covered glass container (Fig. 1).
  • Units: All measurements are in millimeters.
  • Reporting: Final results rounded according to IS 2-1960.

Fundamental Equation:

[ \text{Water Transmission Rate} = \frac{\text{Water loss (g)}}{48 \text{ hours}} ]


Referenced Indian Standards (Appendix A):

IS CodeDescription
IS 1122Determination of specific gravity and porosity
IS 1124Water absorption tests for natural stones
IS 1126Durability evaluation
IS 1706Abrasion resistance assessment

This standard aligns with global practices to reliably assess waterproofing properties of natural stone adhesives.

2Sampling and Selection of Test Samples

Guidance on Sampling Procedures and Criteria

Specifications:

  • Sample Selection (Clauses 2.1 - 2.4):

    • Samples should accurately represent the average stone type or grade.
    • If noticeable variations exist, multiple samples must be chosen to cover the full property range.
  • Sample Weight and Condition (Clause 2.2):

    • Minimum 25 kg of fresh, unweathered stone per sample.
    • Samples must be taken from distinct strata differing in color, texture, or structure.
    • Exclude any damaged or altered stones (e.g., blasted or heated).
  • Field Stones and Boulders (Clause 2.3):

    • Conduct thorough deposit inspections.
    • Document types and conditions of stones.
    • Collect separate samples for each stone class suitable for construction.

Sampling Summary Table

Source CategorySample MassSelection CriteriaRemarks
Quarry or Ledge≥ 25 kgSamples from strata with distinct featuresDamaged stones excluded
Field Stones and Boulders≥ 25 kgSamples from identified stone classesDeposit inspected in detail
flowchart LR
  A[Inspect Quarry/Deposit] --> B{Is Stone Quality Varied?}
  B -- Yes --> C[Collect Multiple Samples from Different Strata]
  B -- No --> D[Collect Single Representative Sample]
  C & D --> E[Ensure Minimum 25 kg of Fresh Stone]
  E --> F[Exclude Damaged Pieces]
  F --> G[Samples Ready for Testing]

This approach ensures representative material for dependable test outcomes.

3Test Specimen Preparation

Specifications and Dimensions for Test Samples

Specimen Dimensions (Clause 3.1):

  • Shape: Square prism
  • Cross-sectional area: 5 cm × 5 cm
  • Length: 6 cm
  • Surface: Square-cut or finely dressed on all faces
  • Orientation: 5×5 cm face aligned parallel to stratification planes

Sampling Notes (Clause 2.4):

  • Multiple specimens must be taken if significant rock quality variation exists to represent the property range.

Weighing Requirements (Clause 4.3):

  • Use a balance with 0.01 g sensitivity for weighing.

Test Setup (Clause 5.1):

  • Place specimen centrally in a glass container.
  • Fill container with distilled water to approximately three-fourths of depth (1.5 cm).
  • Position a cover plate with a central hole over the container.
  • Apply wax coating on the specimen portion above the cover to prevent evaporation.

Summary Table of Specimen Dimensions

ParameterDimension
Cross-section5 cm × 5 cm
Length6 cm
Weighing Accuracy0.01 g
Water Depth in Vessel1.5 cm (75% depth)

flowchart TD
  A[Specimen: 5x5 cm Cross-section] --> B[Square Prism]
  B --> C[Length 6 cm]
  C --> D[Placed in Glass Vessel]
  D --> E[Distilled Water at 1.5 cm Depth]
  E --> F[Cover Plate with Central Aperture]
  F --> G[Wax Coating on Exposed Specimen Surfaces]

This ensures uniform specimen preparation and reliable testing.

4Testing Equipment and Setup

Details of Apparatus for Measuring Water Transmission

  • Glass Vessel:

    • Diameter: 100 mm (10 cm)
    • Depth: 20 mm (2 cm)
    • Material: Shallow glass container with a ground glass flange
  • Cover Plate:

    • Central square aperture: 52.5 mm × 52.5 mm
    • Ground glass flange fitting onto vessel flange
    • Flanges greased to ensure airtight and leak-proof connection
  • Precision Balance:

    • Sensitivity: 0.01 g

Test Assembly (Refer to Fig. 1)

  • Place specimen centrally inside glass vessel.
  • Fill vessel with distilled water up to approximately 15 mm (3/4 depth).
  • Position cover plate so that specimen protrudes through aperture.
  • Apply wax coating on specimen surfaces above cover to prevent evaporation.

Water Transmission Rate Calculation

Water transmission rate (g/48 hours) = Weight loss of water (g) after 48 hours once steady state is reached.


Important Considerations

  • Use distilled water exclusively.
  • Grease ground glass flanges for a sealed, leak-proof setup.
  • Weigh specimens with a precision balance after 48 hours to determine water uptake via capillary action.

flowchart LR
  A[Glass Vessel (10 cm diameter, 2 cm depth)] --> B[Fill with distilled water (1.5 cm depth)]
  B --> C[Place specimen in center]
  C --> D[Cover with plate having 5.25 cm square hole]
  D --> E[Wax coat specimen sides above cover]
  E --> F[Weigh specimen after 48 hours on 0.01 g balance]

This configuration guarantees precise measurement of water transmission per the standard.

5Testing Methodology

Procedure for Measuring Water Transmission Rate through Natural Stones

Key Points:

  • Balance Precision: Use a weighing scale accurate to 0.01 g (Clause 4.3).
  • Materials: Waterproofing adhesive, distilled water, glass vessel with cover.
  • Units: All dimensions in millimeters as per Fig. 1.

Test Steps (Clause 5):

  • Record initial specimen weight.
  • Perform successive weighings every 24 hours to monitor water loss caused by capillary action (Clause 5.5).
  • Apply rounding rules in accordance with IS 2:1960 to final results.

Reporting (Clause 6):

  • Document the water transmission rate by capillary action based on specimen weight loss over the test duration.

Rounding Guidelines (IS 2:1960):

Digit ValueRounding Action
Less than 5Round down
5 or greaterRound up

flowchart TD
  A[Prepare and Condition Specimen] --> B[Weigh Initial Specimen]
  B --> C[Place in Glass Vessel]
  C --> D[Wait 24 Hours]
  D --> E[Weigh Specimen]
  E --> F[Calculate Weight Loss]
  F --> G[Repeat Weighing Every 24 Hours]
  G --> H[Determine Final Water Transmission Rate]

This ensures an accurate evaluation of water movement through stone samples.

6Documentation of Test Findings

Guidelines for Reporting Results

  • Balance Sensitivity: Use a balance with 0.01 g accuracy (Clause 4.3).
  • Weighing Schedule: Weigh specimens every 24 hours to track water loss (Clause 5.5).
  • Water Loss Rate: Report the rate and duration until water loss stabilizes (Clause 6.2).
  • Rounding: Apply IS 2-1960 rounding conventions to the final figures (Clause 6, Note 0.5).

Typical Testing Arrangement (Fig. 1):

  • Distilled water in a covered glass vessel.
  • Measure water loss through the specimen surface.
  • Dimensions specified in millimeters.

Formula for Water Loss Rate

[ \text{Rate} = \frac{\Delta W}{\Delta t} ]

Where:

  • (\Delta W): change in weight (grams)
  • (\Delta t): time interval (hours)

Reporting Summary Table

ParameterSpecification
Balance Precision0.01 g
Weighing IntervalEvery 24 hours
Water TypeDistilled
Vessel ConfigurationGlass container with cover
Rounding StandardIS 2-1960
Report ContentRate of water loss and stabilization period

flowchart LR
  A[Begin Test] --> B[Fill Vessel with Distilled Water]
  B --> C[Position Specimen]
  C --> D[Initial Weighing (W1)]
  D --> E[Wait 24 Hours]
  E --> F[Subsequent Weighing (W2)]
  F --> G[Calculate Weight Difference \(\Delta W = W_1 - W_2\)]
  G --> H[Calculate Rate \(\Delta W / 24\)]
  H --> I{Is Rate Constant?}
  I -- No --> E
  I -- Yes --> J[Prepare and Submit Report]

This procedure enables consistent and precise documentation of water transmission test results.

Appendix AComplementary Indian Standards for Natural Stones

Associated Indian Standards Relevant to Natural Building Stones

IS CodeTest or SpecificationDescription
IS 1122-1957Specific gravity and porosity determinationMeasures stone density and pore volume
IS 1124-1957Water absorption testingQuantifies moisture uptake by stones
IS 1126-1957Durability assessmentEvaluates weather resistance
IS 1706-1960Abrasion resistanceMeasures surface wear resistance

Key Reference from IS 4121 (Clause 6.3):

  • The water transmission rate by capillary action is expressed as the weight of water lost (grams) over 48 hours after stabilization.

Important Notes:

  • These standards collectively assist in assessing strength, durability, and moisture behavior of natural stones.
  • Perform water absorption tests (IS 1124) prior to capillary water transmission testing (IS 4121).
  • Specific gravity and porosity (IS 1122) influence stone durability and moisture movement.

Water Transmission Rate Formula:

[ \text{Water Transmission Rate} = \frac{\text{Water loss (g) after 48 hours}}{\text{Surface area (cm}^2)} ]


This set of Indian Standards provides a thorough framework for evaluating natural stones for construction applications.

Popular Questions About IS 4121

?What are the required dimensions and preparation methods for test specimens?

Dimensions and Preparation for Test Specimens as per IS 4121:

  • Dimensions (Clause 3.1):

    • Cross-section: 5 cm × 5 cm square prism
    • Length: 6 cm
    • Surfaces: Square-cut or finely dressed
    • Orientation: 5×5 cm face aligned with stratification planes
  • Number of Specimens (Clause 3.2): At least six specimens per test

  • Preparation (Clause 5.1):

    • Place the specimen centrally in a glass vessel
    • Fill vessel with distilled water up to three-fourths depth (1.5 cm)
    • Cover vessel with a plate having a central hole for specimen projection
    • Apply wax coating on specimen surfaces above the cover to prevent evaporation
  • Sampling (Clause 2.4): For rocks showing quality variation, take multiple samples to cover the property range

This method ensures uniformity and reliability in specimen testing.

?How is the test apparatus configured to measure water transmission by capillary action?

Configuration of Test Apparatus for Water Transmission by Capillary Action:

  • The natural stone specimen is vertically positioned with its base immersed in distilled water inside a glass vessel.
  • The vessel is covered with a plate having a central aperture through which the specimen protrudes.
  • Waterproofing adhesive is applied around the specimen to prevent lateral water leakage.
  • The specimen absorbs water via capillary action, and its weight gain is periodically measured.
  • A balance with 0.01 g accuracy is used for weighing.

Typical Layout (Fig. 1):

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This setup allows precise determination of water transmission rate according to the standard.

?What environmental conditions must be maintained during the test?

Per IS 4121, the test must be conducted under controlled conditions:

  • Relative Humidity: 65% ± 5%
  • Temperature: 27°C ± 2°C
  • Conditioning: Specimens should be conditioned in this environment for 24 hours prior to testing

These conditions ensure moisture and temperature equilibrium in the specimen for consistent water transmission measurements.

Additional points:

  • The specimen is placed in distilled water filled to about 75% of the vessel depth (1.5 cm).
  • Wax coating is applied above the cover plate to prevent evaporation.
  • Specimens are weighed every 24 hours to record water loss.
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Maintaining these environmental conditions is crucial for reproducible results.

?How is the specimen sealed to prevent water leakage and evaporation?

According to IS 4121, sealing involves:

  • Placing the specimen centrally in a glass vessel filled to approximately three-fourths depth (1.5 cm) with distilled water.
  • Covering the vessel with a plate having a central hole through which the specimen extends.
  • Coating the portion of the specimen above the cover plate with a mixture of paraffin wax and resin (or equivalent) to prevent evaporation.
  • Applying the same wax-resin mixture around the hole and at the interface between vessel and cover to ensure a watertight and leak-proof seal.

This sealing method effectively prevents water loss from leakage or evaporation during testing.

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?How is the water transmission rate calculated and reported according to IS 4121?

The water transmission rate by capillary action is determined as follows:

  • The stone specimen is partially immersed in distilled water, allowing capillary rise.
  • Water absorption is measured by recording the height of water rise (h) at specific time intervals (t).
  • The water transmission rate (W) is calculated as the volume of water absorbed per unit area per unit time.

Conceptual Formula:

[ W = \frac{V}{A \times t} ] where:

  • (V): volume of water absorbed (ml)
  • (A): cross-sectional area in contact with water (cm²)
  • (t): time duration (minutes)

Reporting:

  • Include rate of water rise (height/time) and/or volume absorbed per unit area per time.
  • Provide details on specimen type, dimensions, and testing conditions (temperature, water quality).

This calculation aids in evaluating the stone’s resistance to moisture ingress via capillary action.

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