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Discharge Given Velocity Approach Calculator

Discharge by Approach Velocity Formula:

\[ Q' = v \times (b \times d_f) \]

m/s
m
m

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1. What is Discharge by Approach Velocity?

Discharge by Approach Velocity represents the volumetric flow rate of water transported through a given cross-sectional area, calculated using the approach velocity, channel width, and flow depth.

2. How Does the Calculator Work?

The calculator uses the discharge formula:

\[ Q' = v \times (b \times d_f) \]

Where:

Explanation: The formula calculates the volumetric flow rate by multiplying the flow velocity with the cross-sectional area of the channel.

3. Importance of Discharge Calculation

Details: Accurate discharge calculation is crucial for hydraulic engineering, water resource management, flood prediction, and designing efficient water conveyance systems.

4. Using the Calculator

Tips: Enter velocity in m/s, channel width in meters, and flow depth in meters. All values must be positive numbers greater than zero.

5. Frequently Asked Questions (FAQ)

Q1: What units should be used for input values?
A: Velocity should be in meters per second (m/s), width and depth should be in meters (m) for consistent results in cubic meters per second (m³/s).

Q2: Can this formula be used for any channel shape?
A: This specific formula is designed for rectangular channels. For other channel shapes, different formulas accounting for cross-sectional area are required.

Q3: What is the typical range of discharge values?
A: Discharge values can range from very small (0.001 m³/s) for small streams to very large (thousands of m³/s) for major rivers, depending on the channel size and flow velocity.

Q4: How accurate is this calculation method?
A: The calculation provides a theoretical discharge value. Actual discharge may vary due to factors like channel roughness, turbulence, and flow conditions.

Q5: When is this approach velocity method most appropriate?
A: This method is most appropriate for uniform flow conditions in open channels where the velocity distribution is relatively consistent across the cross-section.

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