Formula Used:
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The Drawdown Given Specific Capacity formula calculates the total drawdown in a well based on the discharge rate and the specific capacity of the well. This is a fundamental calculation in hydrogeology for assessing well performance and aquifer characteristics.
The calculator uses the formula:
Where:
Explanation: This formula demonstrates the inverse relationship between specific capacity and drawdown - higher specific capacity means less drawdown for a given discharge rate.
Details: Accurate drawdown calculation is crucial for well design, determining pumping rates, assessing aquifer performance, and ensuring sustainable groundwater extraction without causing excessive drawdown that could affect nearby wells.
Tips: Enter discharge in cubic meters per second (m³/s) and specific capacity in square meters per second (m²/s). Both values must be positive numbers greater than zero for valid calculation.
Q1: What is specific capacity and how is it measured?
A: Specific capacity is measured by conducting a pumping test where discharge and corresponding drawdown are recorded. It represents the well's productivity per unit of drawdown.
Q2: How does drawdown affect well performance?
A: Excessive drawdown can indicate well inefficiency, aquifer depletion, or interference with nearby wells. It helps determine the optimal pumping rate for sustainable operation.
Q3: What are typical specific capacity values?
A: Specific capacity varies widely depending on aquifer characteristics. High-yield aquifers may have specific capacities exceeding 1 m²/s, while low-yield aquifers may be below 0.1 m²/s.
Q4: Can this formula be used for all well types?
A: This formula is generally applicable for most pumping wells, but may need modification for complex aquifer systems, confined vs unconfined aquifers, or wells with screen limitations.
Q5: How does time affect drawdown calculations?
A: This formula gives steady-state drawdown. For time-dependent drawdown analysis, more complex equations like Theis or Jacob equations are required that account for aquifer storage and time since pumping began.