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Constant Depression Head in a well refers to the steady-state drawdown or lowering of the water level when the discharge from the well is constant. It is a key parameter in hydrogeology for assessing well performance and aquifer characteristics.
The calculator uses the formula:
Where:
Explanation: This formula calculates the constant depression head by dividing the discharge rate by the product of the cross-sectional area and the specific capacity of the well.
Details: Calculating constant depression head is essential for well design, determining well efficiency, and understanding aquifer properties. It helps in predicting water level drawdown under various pumping conditions.
Tips: Enter discharge in m³/s, cross-sectional area in m², and specific capacity in m/s. All values must be positive numbers greater than zero.
Q1: What is specific capacity in well hydraulics?
A: Specific capacity is a measure of well productivity, defined as the discharge per unit drawdown (Q/s). It indicates how much water a well can produce for a given amount of drawdown.
Q2: How does cross-sectional area affect depression head?
A: Larger cross-sectional areas typically result in smaller depression heads for the same discharge, as the flow is distributed over a larger area.
Q3: What are typical units for these measurements?
A: Discharge is typically measured in m³/s or L/s, cross-sectional area in m², specific capacity in m/s or m²/s, and depression head in meters.
Q4: When is constant depression head assumption valid?
A: This assumption is valid in steady-state conditions when the pumping rate has been constant long enough for water levels to stabilize.
Q5: How does this relate to well efficiency?
A: Constant depression head calculations help determine well efficiency by comparing theoretical drawdown with actual measured drawdown under pumping conditions.