Formula Used:
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The Pumping Rate from Distance Drawdown Graphs calculation determines the volume of water pumped per unit time based on aquifer transmissivity and drawdown measurements. This is essential for groundwater resource management and well performance analysis.
The calculator uses the formula:
Where:
Explanation: This formula calculates the pumping rate by considering the aquifer's ability to transmit water and the observed drawdown across a logarithmic cycle.
Details: Accurate pumping rate estimation is crucial for sustainable groundwater extraction, well design, aquifer testing, and managing water resources effectively.
Tips: Enter transmissivity in m²/s and drawdown across log cycle in meters. All values must be positive numbers greater than zero.
Q1: What is transmissivity in groundwater hydrology?
A: Transmissivity measures how much water can be transmitted horizontally through an aquifer unit width under a unit hydraulic gradient.
Q2: How is drawdown across log cycle measured?
A: Drawdown across log cycle is determined from time-drawdown or distance-drawdown graphs by measuring the change in drawdown over one log cycle.
Q3: What are typical pumping rate units?
A: While m³/s is used here, pumping rates are often expressed in L/s, m³/h, or gallons per minute (GPM) depending on the application.
Q4: When is this calculation most applicable?
A: This method is particularly useful for analyzing pumping test data and determining sustainable extraction rates from aquifers.
Q5: What factors can affect pumping rate accuracy?
A: Aquifer heterogeneity, well efficiency, boundary conditions, and measurement errors can all impact the accuracy of pumping rate calculations.