Dicken's Formula:
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Dicken's Constant refers to an empirical coefficient used in Dicken's formula to estimate peak flood discharge based on the area of the catchment. In India, this constant typically ranges from 11 to 14, depending on regional characteristics and catchment conditions.
The calculator uses Dicken's formula:
Where:
Explanation: The formula calculates the empirical constant used in flood discharge estimation by relating the peak flood discharge to the catchment area raised to the power of 3/4.
Details: Dicken's Constant is crucial for flood estimation in hydrology and civil engineering. It helps in designing drainage systems, flood control structures, and water resource management by providing a reliable method to estimate peak flood discharges based on catchment characteristics.
Tips: Enter flood discharge in cubic meters per second (m³/s) and catchment area in square kilometers (km²). Both values must be positive numbers greater than zero for accurate calculation.
Q1: What is the typical range of Dicken's Constant?
A: In India, Dicken's Constant typically ranges from 11 to 14, though it may vary based on regional topography and rainfall patterns.
Q2: How does catchment area affect Dicken's Constant?
A: Larger catchment areas generally result in different constant values due to varying hydrological responses and flow characteristics.
Q3: When should Dicken's formula be used?
A: Dicken's formula is particularly useful for preliminary flood estimation in regions where detailed hydrological data is limited.
Q4: Are there limitations to Dicken's formula?
A: Yes, the formula is empirical and may not account for all local factors such as soil type, vegetation cover, and rainfall intensity variations.
Q5: How accurate is Dicken's formula compared to other methods?
A: While useful for quick estimates, more sophisticated hydrological models should be used for critical infrastructure design where precise flood estimation is required.