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Volume Of Water Drained By Gravity Given Specific Yield Calculator

Formula Used:

\[ W_y = \frac{\%S_y \times V}{100} \]

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1. What is Volume Of Water Drained By Gravity?

Volume of water drained by gravity is defined as the quantity of water that is drained by gravity from a saturated aquifer or soil mass when subjected to gravity drainage.

2. How Does the Calculator Work?

The calculator uses the formula:

\[ W_y = \frac{\%S_y \times V}{100} \]

Where:

Explanation: The formula calculates the volume of water that can be extracted by gravity drainage from a given total volume of aquifer material, based on its specific yield percentage.

3. Importance of Calculation

Details: Accurate calculation of water volume drained by gravity is crucial for groundwater resource management, well yield estimation, and designing effective drainage systems in hydrogeology and civil engineering projects.

4. Using the Calculator

Tips: Enter specific yield percentage (as a positive number) and total volume in cubic meters. Both values must be greater than zero for accurate calculation.

5. Frequently Asked Questions (FAQ)

Q1: What is Specific Yield Percentage?
A: Specific Yield Percentage tells how much water is available for consumptive use from an aquifer or soil mass when drained by gravity.

Q2: How does Specific Yield differ from Porosity?
A: While porosity measures total void space, specific yield measures only the portion that drains freely under gravity, excluding water retained by capillary forces.

Q3: What are typical Specific Yield values?
A: Specific yield values typically range from 5% to 30% depending on the aquifer material, with coarse sands and gravels having higher values than fine-grained materials.

Q4: When is this calculation most useful?
A: This calculation is particularly useful in groundwater modeling, well design, and estimating sustainable yield from aquifers.

Q5: Are there limitations to this formula?
A: The formula assumes homogeneous material properties and may not account for complex geological formations or time-dependent drainage characteristics.

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