What it is
A steady difference in water level is applied across a saturated specimen and the flow volume is measured.
SANAS T1018
Public test guide
Measures water flow through a relatively permeable soil while a constant hydraulic head is maintained.
Plain-language explanation
The project specification controls the exact method and acceptance requirement.
A steady difference in water level is applied across a saturated specimen and the flow volume is measured.
Prepared specimen, constant-head permeameter, water supply, measuring cylinder, timer and thermometer.
The coefficient of permeability under steady-flow conditions.
Commonly used for sands and gravels in drainage, filter and seepage assessments.
Typical test sequence
Prepare and saturate the specimen
Establish steady flow at the specified head
Measure flow, time and geometry to calculate permeability
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