Formula Used:
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The Coefficient of Permeability at 20° C refers to the measure of a porous medium's ability to allow fluid flow through its voids. It quantifies how easily a fluid can move through a porous material under a hydraulic gradient.
The calculator uses the formula:
Where:
Explanation: This formula converts intrinsic permeability (a property of the porous medium alone) to coefficient of permeability (which depends on both the medium and the fluid properties).
Details: Accurate permeability calculation is crucial for groundwater flow analysis, soil mechanics, petroleum engineering, and environmental studies involving fluid transport through porous media.
Tips: Enter intrinsic permeability in m², unit weight of fluid in N/m³, and dynamic viscosity in Pa·s. All values must be positive and valid.
Q1: What is the difference between intrinsic permeability and coefficient of permeability?
A: Intrinsic permeability is a property of the porous medium alone, while coefficient of permeability depends on both the medium and the fluid properties.
Q2: Why is the calculation done at 20° C?
A: 20° C is a standard reference temperature for fluid properties, particularly for water, which is commonly used in permeability studies.
Q3: What are typical values for coefficient of permeability?
A: Values range from 10⁻² m/s for gravel to 10⁻⁹ m/s for clay, depending on the porous material.
Q4: How does fluid viscosity affect permeability?
A: Higher viscosity fluids experience more resistance to flow, resulting in lower coefficient of permeability values.
Q5: Can this formula be used for gases?
A: While the basic relationship holds, gas permeability calculations often require additional corrections for compressibility and other gas-specific effects.