Formula Used:
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The Specific Gravity of Particle is the ratio of density of particle to density of standard material. It is a dimensionless quantity that indicates how dense a particle is compared to a reference substance (typically water).
The calculator uses the formula:
Where:
Explanation: This formula calculates the specific gravity of particles based on their maximum critical scour velocity, gravitational acceleration, and particle diameter.
Details: Calculating specific gravity is crucial in sediment transport studies, hydraulic engineering, and environmental science. It helps determine particle behavior in fluid flows and is essential for designing erosion control measures and sediment management systems.
Tips: Enter maximum critical scour velocity in m/s, acceleration due to gravity in m/s² (default is 9.8 m/s²), and diameter of particle in meters. All values must be positive numbers.
Q1: What is maximum critical scour velocity?
A: Maximum critical scour velocity is the highest flow velocity at which sediment particles begin to move or be eroded from a surface.
Q2: Why is specific gravity important in sediment transport?
A: Specific gravity determines how easily particles can be transported by fluid flows. Higher specific gravity particles require higher flow velocities to be moved.
Q3: What is the typical range of specific gravity for sediment particles?
A: Most natural sediment particles have specific gravity values between 2.5 and 2.7, with quartz sand typically around 2.65.
Q4: Can this formula be used for all types of particles?
A: This formula works best for spherical or near-spherical particles. Irregularly shaped particles may require additional correction factors.
Q5: How does particle diameter affect the specific gravity calculation?
A: Larger diameter particles generally result in lower specific gravity values when other parameters remain constant, as they require higher velocities to be moved.