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Recharge From Rainfall In Hard Rock Areas With Weathered Basalt Calculator

Formula Used:

\[ R_{wb} = 5 \times A_{cr} \times P_{nm} \]

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1. What is Rainfall Recharge in Hard Rock Weathered Basalt?

The Rainfall Recharge in Hard Rock Weathered Basalt refers to the process by which rainwater infiltrates through the weathered layers of basalt rock and replenishes groundwater reserves. This calculation is essential for managing water resources in hard rock regions.

2. How Does the Calculator Work?

The calculator uses the formula:

\[ R_{wb} = 5 \times A_{cr} \times P_{nm} \]

Where:

Explanation: The formula calculates the amount of water that infiltrates through weathered basalt layers during monsoon season, helping estimate groundwater replenishment.

3. Importance of Rainfall Recharge Calculation

Details: Accurate rainfall recharge estimation is crucial for sustainable groundwater management, water resource planning, and ensuring adequate water supply in hard rock regions.

4. Using the Calculator

Tips: Enter the area of computation in square meters and normal rainfall in meters during monsoon season. All values must be positive numbers.

5. Frequently Asked Questions (FAQ)

Q1: What is the significance of the coefficient 5 in the formula?
A: The coefficient 5 represents the recharge factor specific to weathered basalt formations, accounting for infiltration characteristics of this rock type.

Q2: How is the area of computation determined?
A: The area of computation is typically the catchment area where rainfall contributes to groundwater recharge through weathered basalt layers.

Q3: What time period does "normal rainfall" refer to?
A: Normal rainfall typically refers to the statistical average measured over a 30-year period during monsoon months in a specific region.

Q4: Are there limitations to this calculation method?
A: This method provides an estimate and may need adjustment based on local geological conditions, soil types, and actual infiltration rates.

Q5: How accurate is this recharge estimation?
A: While useful for preliminary assessment, detailed hydrological studies with field measurements provide more accurate recharge estimates.

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