Formula Used:
From: | To: |
The calculation determines the thickness of a confined aquifer during pumping conditions using the discharge rate, permeability coefficient, aquifer characteristics, and well geometry parameters.
The calculator uses the formula:
Where:
Explanation: The formula calculates the effective aquifer thickness during pumping conditions based on the relationship between discharge, permeability, and geometric parameters.
Details: Accurate calculation of aquifer thickness during pumping is crucial for groundwater resource assessment, well design, and predicting the behavior of confined aquifers under extraction conditions.
Tips: Enter all values in appropriate units. Ensure that Radius of Influence is greater than Radius of well. All values must be positive numbers.
Q1: What is a confined aquifer?
A: A confined aquifer is an aquifer that is bounded above and below by impermeable layers, creating pressure conditions that affect water flow.
Q2: Why is the logarithm base 10 used in this formula?
A: Base 10 logarithms are commonly used in hydrogeological calculations as they provide convenient scaling for the large range of values typically encountered.
Q3: What factors affect the coefficient of permeability?
A: The coefficient of permeability depends on the properties of the aquifer material, including grain size, sorting, porosity, and degree of saturation.
Q4: How is radius of influence determined?
A: Radius of influence is typically determined through field measurements, observation wells, or estimated based on pumping test data and aquifer characteristics.
Q5: What are typical values for these parameters?
A: Discharge rates vary from 0.001 to 1 m³/s, permeability from 10⁻⁹ to 10⁻³ m/s, aquifer thickness from 1 to 100+ meters, and well radii from 0.1 to 1 meter.