Formula Used:
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The radius of well calculation determines the distance from the center of a well to its outer boundary based on aquifer properties and pumping conditions. This is essential for well design and groundwater resource management.
The calculator uses the formula:
Where:
Explanation: This formula calculates the well radius based on the relationship between the radius of influence, transmissibility coefficient, aquifer thickness, water depth, and initial discharge rate.
Details: Accurate well radius calculation is crucial for proper well design, determining optimal pumping rates, assessing aquifer yield potential, and ensuring sustainable groundwater extraction.
Tips: Enter all values in appropriate units (meters for lengths, m²/s for transmissibility, m³/s for discharge). Ensure all values are positive and physically meaningful (water depth should not exceed aquifer thickness).
Q1: What is the coefficient of transmissibility?
A: The coefficient of transmissibility represents the rate of water flow through a vertical strip of aquifer under unit hydraulic gradient.
Q2: How is radius of influence determined?
A: Radius of influence is typically measured from pumping test data or estimated based on aquifer properties and pumping conditions.
Q3: Why is base 10 used in this formula?
A: Base 10 logarithms are commonly used in groundwater equations due to historical conventions and ease of calculation.
Q4: What are typical values for well radius?
A: Well radius typically ranges from 0.1 to 0.5 meters for most water supply wells, depending on the well construction and purpose.
Q5: When should this calculation be used?
A: This calculation is used during well design phase, aquifer testing analysis, and groundwater resource evaluation projects.