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Time Interval At Inter-Isochrone Area Given Inflow Calculator

Time Interval Formula:

\[ \Delta t = 2.78 \times \frac{Ar}{I} \]

m³/s

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1. What is the Time Interval Formula?

The Time Interval formula calculates the time required for hydrological changes based on inter-isochrone area and inflow rate. It's commonly used in watershed management and flood prediction studies to determine translation times of runoff.

2. How Does the Calculator Work?

The calculator uses the Time Interval formula:

\[ \Delta t = 2.78 \times \frac{Ar}{I} \]

Where:

Explanation: The formula calculates the time interval by multiplying the constant 2.78 with the ratio of inter-isochrone area to inflow rate.

3. Importance of Time Interval Calculation

Details: Accurate time interval calculation is crucial for watershed management, flood prediction, and hydrological modeling. It helps in understanding runoff translation times and planning appropriate water management strategies.

4. Using the Calculator

Tips: Enter inter-isochrone area in square meters and inflow rate in cubic meters per second. Both values must be positive numbers greater than zero.

5. Frequently Asked Questions (FAQ)

Q1: What is inter-isochrone area?
A: Inter-isochrone area divides a watershed into subareas with distinct runoff translation times, helping in hydrological analysis and flood prediction.

Q2: Why is the constant 2.78 used in the formula?
A: The constant 2.78 is a conversion factor that accounts for unit conversions and empirical relationships in hydrological calculations.

Q3: What are typical values for inflow rate?
A: Inflow rates vary significantly based on watershed characteristics, rainfall intensity, and land use. They can range from small fractions to hundreds of cubic meters per second.

Q4: Can this formula be used for all watershed types?
A: While generally applicable, the formula may need adjustments for extremely large or small watersheds, or those with unique hydrological characteristics.

Q5: How accurate is this calculation method?
A: The method provides a good estimate for most practical purposes, but for critical applications, more detailed hydrological modeling may be required.

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