Water Pressure Equation:
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Water pressure at depth refers to the pressure exerted by a column of water at a specific depth below the surface. It increases with depth due to the weight of the water above.
The calculator uses the hydrostatic pressure equation:
Where:
Explanation: The pressure increases linearly with depth and depends on the density of the fluid and the gravitational acceleration.
Details: Calculating water pressure is essential for designing underwater structures, diving safety, hydraulic systems, and understanding fluid dynamics in various engineering applications.
Tips: Enter fluid density in kg/m³ (1000 for pure water), gravitational acceleration in m/s² (9.81 on Earth), and depth in meters. All values must be positive.
Q1: Why does pressure increase with depth?
A: Pressure increases with depth because the weight of the fluid above adds to the pressure at deeper levels.
Q2: Does this equation work for all fluids?
A: Yes, the equation works for any fluid, but you must use the correct density value for that specific fluid.
Q3: How does salinity affect water pressure calculations?
A: Saltwater has a higher density than freshwater (approximately 1025 kg/m³ vs 1000 kg/m³), which results in slightly higher pressure at the same depth.
Q4: What is the pressure at 10 meters depth in freshwater?
A: Using ρ = 1000 kg/m³, g = 9.81 m/s², h = 10 m: P = 1000 × 9.81 × 10 = 98,100 Pa or approximately 0.97 atmospheres.
Q5: How is this different from atmospheric pressure?
A: This calculation gives the pressure due to the water column only. Total pressure at depth would be this water pressure plus the atmospheric pressure at the surface.