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Time Given Formation Constant S Calculator

Formula Used:

\[ \text{Time in Days} = \frac{\text{Formation Constant S}}{\frac{4 \times \text{Well Function Constant} \times \text{Formation Constant T}}{\text{Radial Distance}^2}} \]

m²/s
m

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1. What is the Time Given Formation Constant S Formula?

The Time Given Formation Constant S formula calculates the time in days based on formation constants and radial distance. It is used in hydrogeological studies to determine time parameters in aquifer testing and analysis.

2. How Does the Calculator Work?

The calculator uses the formula:

\[ \text{Time in Days} = \frac{\text{Formation Constant S}}{\frac{4 \times \text{Well Function Constant} \times \text{Formation Constant T}}{\text{Radial Distance}^2}} \]

Where:

Explanation: The formula calculates time based on the relationship between formation constants and radial distance in hydrogeological systems.

3. Importance of Time Calculation

Details: Accurate time calculation is crucial for aquifer characterization, groundwater flow analysis, and well testing interpretation in hydrogeological studies.

4. Using the Calculator

Tips: Enter all values as positive numbers. Formation Constant T should be in m²/s and Radial Distance in meters. All values must be greater than zero.

5. Frequently Asked Questions (FAQ)

Q1: What are typical values for Formation Constants?
A: Formation constants vary widely depending on the aquifer material and conditions, typically ranging from 0.001 to 10 m²/s for Formation Constant T.

Q2: How is Radial Distance measured?
A: Radial distance is measured from the center of the well to the point of observation in the aquifer.

Q3: What units does this calculator use?
A: The calculator uses SI units: meters for distance, m²/s for Formation Constant T, and days for time.

Q4: When is this formula typically applied?
A: This formula is commonly used in pumping test analysis and aquifer characterization studies.

Q5: Are there limitations to this calculation?
A: The calculation assumes ideal aquifer conditions and may need adjustment for heterogeneous aquifers or complex boundary conditions.

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