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Formation Constant T Given Formation Constant S Calculator

Formula Used:

\[ T = \frac{Fc}{\left( \frac{4 \times u \times t_{days}}{d_{radial}^2} \right)} \]

m²/s
days
m

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1. What Is Formation Constant T?

Formation Constant T is an equilibrium constant for the formation of a complex in solution, measured in square meters per second (m²/s). It represents the transmissivity of an aquifer formation.

2. How Does The Calculator Work?

The calculator uses the formula:

\[ T = \frac{Fc}{\left( \frac{4 \times u \times t_{days}}{d_{radial}^2} \right)} \]

Where:

Explanation: This formula calculates the formation constant T based on unsteady flow conditions, well function characteristics, time duration, and radial distance from the well.

3. Importance Of Formation Constant Calculation

Details: Accurate calculation of Formation Constant T is crucial for groundwater flow analysis, aquifer characterization, and well design in hydrogeological studies.

4. Using The Calculator

Tips: Enter all values with appropriate units. Formation constants and time should be positive values. Radial distance must be greater than zero.

5. Frequently Asked Questions (FAQ)

Q1: What is the significance of Formation Constant T?
A: Formation Constant T represents the transmissivity of an aquifer, indicating how easily water can move through the geological formation.

Q2: How does radial distance affect the calculation?
A: Radial distance is squared in the denominator, meaning it has a significant impact on the result. Larger distances result in smaller calculated T values.

Q3: What is the Well Function Constant?
A: The Well Function Constant (u) is a dimensionless parameter that depends on the specific characteristics of the well function being used in the analysis.

Q4: Can this calculator be used for steady-state flow?
A: No, this specific formula is designed for unsteady flow conditions where time is a factor in the calculation.

Q5: What are typical ranges for Formation Constant T values?
A: T values vary widely depending on aquifer material, ranging from 0.0001 m²/s for clay to 0.1 m²/s or more for highly permeable gravel aquifers.

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