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Area Of Aquifer Given Rate Of Change Of Volume Calculator

Formula Used:

\[ Aquifer Area = \frac{Rate\ of\ Change\ of\ Volume}{(Rate\ of\ Change\ of\ Height) \times Storage\ Coefficient} \] \[ A_{aq} = \frac{\frac{\delta V}{\delta t}}{(\frac{\delta h}{\delta t}) \times S} \]

cm³/s
m/s

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1. What is Aquifer Area Calculation?

The aquifer area calculation determines the saturated area beneath the water table using the relationship between volume change, height change, and storage coefficient. This is essential in hydrogeology for understanding groundwater resources and aquifer characteristics.

2. How Does the Calculator Work?

The calculator uses the formula:

\[ A_{aq} = \frac{\frac{\delta V}{\delta t}}{(\frac{\delta h}{\delta t}) \times S} \]

Where:

Explanation: The formula calculates the aquifer area by dividing the rate of volume change by the product of rate of height change and storage coefficient.

3. Importance of Aquifer Area Calculation

Details: Accurate aquifer area calculation is crucial for groundwater resource management, well field design, contaminant transport studies, and sustainable water extraction planning.

4. Using the Calculator

Tips: Enter rate of change of volume in cm³/s, rate of change of height in m/s, and storage coefficient (dimensionless). All values must be positive numbers.

5. Frequently Asked Questions (FAQ)

Q1: What is the storage coefficient?
A: The storage coefficient is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer.

Q2: Why are different units used for volume and height changes?
A: The formula accommodates standard units used in hydrogeological measurements, where volume changes are often measured in cm³ and height changes in meters.

Q3: What is a typical range for storage coefficient?
A: Storage coefficient typically ranges from 0.0001 to 0.001 for confined aquifers and 0.1 to 0.3 for unconfined aquifers.

Q4: How accurate is this calculation?
A: The accuracy depends on the precision of input measurements and the assumption of homogeneous aquifer properties.

Q5: Can this formula be used for all aquifer types?
A: This formula is generally applicable but may need modifications for complex aquifer systems or anisotropic conditions.

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