2500 cm3 of water was measured in 120 minutes for the experiment from a sample with a diameter of 15 cm and a length of 30 cm, on which the constant level permeability test was performed. There is a height difference of 2.5m between the level from which the water is taken and the fixed water level. Find the permeability coefficient of the test sample? (π=3.14) will be taken

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Laboratory Determination of Hydraulic Conductivity

Hydraulic conductivity is the measure of flowability of water inside the soil in the presence of a hydraulic gradient. The hydraulic gradient is defined as the difference in the water heads in the soil, which induces a water motion. In simple terms, a hydraulic gradient is the presence of a potential that induces a flow of water.