Specific Gravity of Sediment Formula:
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Specific Gravity of Sediment is the ratio of the density of sediment particles to the density of water. It provides important information about the relative weight of sediment particles compared to water.
The calculator uses the formula:
Where:
Explanation: This formula calculates the specific gravity of sediment particles based on their settling velocity, diameter, and drag characteristics in fluid.
Details: Calculating specific gravity of sediment is crucial for understanding sediment transport, erosion processes, and designing effective sediment control measures in hydraulic engineering.
Tips: Enter settling velocity in m/s, acceleration due to gravity in m/s² (default 9.8), diameter in meters, and coefficient of drag. All values must be positive.
Q1: What is the typical range for specific gravity of sediment?
A: Most natural sediments have specific gravity values between 2.5-2.7, with quartz sand typically around 2.65.
Q2: How does particle shape affect the coefficient of drag?
A: Spherical particles have lower drag coefficients than irregularly shaped particles, which experience more resistance when settling.
Q3: Why is specific gravity important in sediment transport?
A: Specific gravity directly influences the settling velocity and transportability of sediment particles in flowing water.
Q4: Can this formula be used for all particle sizes?
A: The formula works best for spherical particles and may require adjustments for highly irregular shapes or very fine particles.
Q5: How does temperature affect the calculation?
A: Temperature affects water density and viscosity, which indirectly influence settling velocity and should be considered for precise calculations.