Formula Used:
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Drawdown Given Well Loss refers to the total reduction in hydraulic head observed at a well, which includes both aquifer loss and head loss within the well system. This measurement is crucial in hydrogeology for assessing well performance and aquifer characteristics.
The calculator uses the formula:
Where:
Explanation: The equation accounts for both the loss due to aquifer properties and the additional head loss that occurs within the well structure itself.
Details: Accurate drawdown calculation is essential for determining well efficiency, designing pumping systems, and assessing aquifer sustainability. It helps in optimizing well performance and preventing over-extraction of groundwater resources.
Tips: Enter the aquifer loss (BQ) and head loss in wells (CQ^n) values in meters. Both values must be non-negative numbers representing valid hydraulic measurements.
Q1: What is the difference between aquifer loss and well loss?
A: Aquifer loss occurs due to the resistance of the aquifer material to water flow, while well loss results from turbulence and friction within the well structure and screen.
Q2: How do I measure aquifer loss and well loss separately?
A: These are typically determined through step-drawdown tests where multiple pumping rates are used to differentiate between aquifer characteristics and well efficiency factors.
Q3: What are typical values for drawdown in wells?
A: Drawdown values vary significantly based on aquifer properties, well design, and pumping rates. They can range from a few centimeters to several meters depending on specific conditions.
Q4: Why is it important to calculate total drawdown accurately?
A: Accurate drawdown calculation helps determine the optimal pumping rate, assess well efficiency, and prevent issues such as well deterioration or aquifer depletion.
Q5: Can this calculator be used for all types of wells?
A: The basic principle applies to most well types, but specific coefficients and exponents may vary based on well construction, aquifer type, and local hydrogeological conditions.