Fuller's Formula:
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Fuller's Constant refers to an empirical coefficient used in Fuller's formula to estimate peak flood discharge, adjusted for regional hydrological conditions. It is a crucial parameter in flood discharge calculations that accounts for catchment characteristics and regional variations.
The calculator uses Fuller's formula:
Where:
Explanation: The formula calculates Fuller's Constant based on flood discharge, catchment area, and time period, incorporating logarithmic relationships and area-dependent coefficients.
Details: Fuller's Constant is essential for accurate flood discharge estimation in hydrological studies. It helps in designing flood control structures, urban drainage systems, and water resource management by providing region-specific coefficients that improve prediction accuracy.
Tips: Enter flood discharge in m³/s, catchment area in m², and time period in seconds. All values must be positive and valid for accurate calculation of Fuller's Constant.
Q1: What is the typical range of Fuller's Constant values?
A: Fuller's Constant typically ranges between 0.1 to 0.3, but can vary significantly based on regional hydrological characteristics and catchment properties.
Q2: How does catchment area affect Fuller's Constant?
A: Larger catchment areas generally result in smaller Fuller's Constant values due to the inverse relationship in the formula, reflecting the distributed nature of runoff in larger basins.
Q3: Why is Napier's constant (e) used in the formula?
A: Napier's constant is used as the base for the logarithmic function to model the exponential decay relationship between time period and flood discharge characteristics.
Q4: Can this constant be used for all types of catchments?
A: While Fuller's formula is widely applicable, the constant may need regional calibration for specific catchment types, particularly in areas with unusual geological or climatic conditions.
Q5: How accurate is Fuller's Constant for flood prediction?
A: Fuller's Constant provides good accuracy for most practical applications when properly calibrated, though it should be used with other methods for critical flood risk assessments.