IS 4121

: 1967

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

CurrentSpecializedTesting MethodMaterials Science · Stones
Download PDFBIS PortalGoogle

This standard lays down the procedure to determine the rate of water transmission through natural building stones via capillary action. It is essential for evaluating a stone's susceptibility to rising dampness, porosity, and long-term weathering resistance.

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

Quick Reference Values
Drying temperature105 ± 5 °C
Accuracy of weighing balance0.01 g
Immersion depth of specimen base3 to 5 mm
Key Formulas
Water transmission rate = (M2 - M1) / (A * t) — Rate of water absorbed per unit area over time
Practical Notes
Testing should be performed relative to the natural bedding plane of the stone, as capillary absorption is often highly anisotropic.
Ensure the test environment is free from drafts and direct sunlight to prevent premature evaporation from the stone's upper surfaces.
The stone must reach a constant mass during the oven-drying phase to ensure all residual moisture is eliminated before the test begins.