Coefficient of Permeability Formula:
Definition: The Coefficient of Permeability (k) describes how easily a liquid will move through soil or porous medium.
Purpose: It's crucial for designing earth dams, assessing groundwater flow, and analyzing seepage in geotechnical engineering.
The calculator uses the formula:
Where:
Explanation: The coefficient is derived from the square root of the product of intrinsic permeability and relative permeability.
Details: Proper permeability calculation ensures dam stability, controls seepage, and prevents piping failures in earth dams.
Tips: Enter intrinsic permeability (Ko) in m², relative permeability (μr) in H/m, and tolerance percentage (default ±5%). All values must be > 0.
Q1: What is intrinsic permeability?
A: It's a measure of how easily a porous medium can transmit fluid, depending only on the medium's structure.
Q2: How does relative permeability differ?
A: Relative permeability compares a fluid's permeability at partial saturation to its permeability at full saturation.
Q3: Why include tolerance?
A: Tolerance (±5% default) accounts for material variability and measurement uncertainties in real-world conditions.
Q4: Typical values for earth dams?
A: For clay cores: 10-9 to 10-7 m/s; for shell materials: 10-5 to 10-3 m/s.
Q5: How to measure these parameters?
A: Laboratory tests like constant-head or falling-head permeability tests for k, specialized equipment for Ko and μr.