Coefficient of Permeability in Well Hydraulics Formula:
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The Coefficient of Permeability in Well Hydraulics describes how easily a liquid will move through the soil. It is a crucial parameter in groundwater hydrology that quantifies the ability of an aquifer to transmit water.
The calculator uses the formula:
Where:
Explanation: This formula calculates the permeability coefficient based on well hydraulics principles, considering the geometric and flow characteristics of the aquifer system.
Details: Accurate determination of permeability coefficient is essential for groundwater resource management, well design, contaminant transport studies, and predicting aquifer response to pumping.
Tips: Enter all values in appropriate units (meters for length, m³/s for discharge). Ensure all values are positive and the radius of influence is greater than the well radius for valid results.
Q1: What is the typical range of permeability coefficients?
A: Permeability coefficients vary widely from 10⁻¹² m/s for clay to 10⁻² m/s for gravel, depending on soil type and composition.
Q2: How does aquifer thickness affect permeability?
A: Aquifer thickness directly influences the transmissivity of the aquifer, which is the product of permeability coefficient and aquifer thickness.
Q3: What factors can affect the accuracy of this calculation?
A: Well construction, aquifer heterogeneity, boundary conditions, and measurement errors can affect the accuracy of permeability calculations.
Q4: When is this formula most applicable?
A: This formula is particularly useful for confined aquifers with radial flow to a fully penetrating well under steady-state conditions.
Q5: How does drawdown relate to permeability?
A: Lower permeability results in greater drawdown for the same pumping rate, as water moves more slowly through the aquifer material.