Formula Used:
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Excursion Amplitude of Fluid Particles in oscillatory flow is defined as a parameter influencing the sediment transport under water waves. It represents the maximum displacement of fluid particles in oscillatory motion.
The calculator uses the formula:
Where:
Explanation: The formula calculates the maximum displacement of fluid particles by multiplying the displacement parameter with the length scale.
Details: Accurate calculation of excursion amplitude is crucial for understanding sediment transport mechanisms, coastal erosion patterns, and designing effective coastal protection structures.
Tips: Enter the displacement parameter and length scale values. Both values must be positive numbers. The result will be the excursion amplitude in meters.
Q1: What is oscillatory flow?
A: Oscillatory flow refers to the back-and-forth motion of fluid particles, commonly observed in wave-induced water movements in coastal environments.
Q2: How does excursion amplitude affect sediment transport?
A: Larger excursion amplitudes typically result in greater sediment movement as fluid particles travel longer distances during each oscillation cycle.
Q3: What are typical values for displacement parameter?
A: The displacement parameter varies depending on wave conditions and sediment characteristics, typically ranging from 0.1 to 2.0 in coastal engineering applications.
Q4: Can this calculator be used for all types of oscillatory flows?
A: This calculator is specifically designed for sediment transport under water waves in coastal engineering contexts.
Q5: What units should be used for input values?
A: The displacement parameter is dimensionless, while length scale should be entered in meters (m).