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Quantity of water measured (Given cross-sectional area, hydraulic conductivity, difference of hydraulic and length )
Formula
Q
the quantity of water flowing through the soil specimen
A
cross-sectional area of the specimen
h
the difference of hydraulic head over distance L
Formula description
Hydraulic conductivity is a property of vascular plants, soil or rock, which describes the ease with which water can move through pore spaces or fractures. This procedure allows water to move through the soil under a steady state head condition while the quantity (volume) of water flowing through the soil specimen is measured over a period of time.