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Discharge For Fully Penetrating Well Given Correction Factor Calculator

Formula Used:

\[ \text{Discharge in Enviro. Engin.} = \frac{\text{Discharge for Partially Penetrating Well}}{\text{Correction Factor}} \] \[ Q_{ee} = \frac{Q_v}{G} \]

m³/s
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1. What is the Discharge Formula?

The discharge formula calculates the environmental engineering discharge for a fully penetrating well by dividing the discharge for a partially penetrating well by a correction factor. This accounts for differences in well penetration and flow characteristics.

2. How Does the Calculator Work?

The calculator uses the formula:

\[ Q_{ee} = \frac{Q_v}{G} \]

Where:

Explanation: The formula adjusts the discharge from a partially penetrating well to estimate what the discharge would be for a fully penetrating well under similar conditions.

3. Importance of Discharge Calculation

Details: Accurate discharge calculation is crucial for groundwater resource management, well design, and environmental impact assessments of water extraction projects.

4. Using the Calculator

Tips: Enter the discharge for partially penetrating well in m³/s and the correction factor. Both values must be positive numbers greater than zero.

5. Frequently Asked Questions (FAQ)

Q1: What is a correction factor in this context?
A: The correction factor accounts for the reduced flow efficiency of a partially penetrating well compared to a fully penetrating one.

Q2: How is the correction factor determined?
A: The correction factor is typically determined through field tests, analytical solutions, or numerical modeling based on well geometry and aquifer properties.

Q3: What are typical values for the correction factor?
A: Correction factors typically range from 1.0 to 2.0, with values closer to 1.0 indicating minimal penetration effects.

Q4: When is this calculation most useful?
A: This calculation is particularly useful when comparing well performance or estimating the potential yield of a fully penetrating well based on data from partially penetrating test wells.

Q5: Are there limitations to this formula?
A: The formula assumes homogeneous aquifer conditions and may not accurately represent complex geological settings or anisotropic aquifers.

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