Water Density Formula:
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Definition: This calculator estimates water density based on pressure using the compressibility equation.
Purpose: It helps engineers and scientists understand how water density changes under different pressure conditions.
The calculator uses the formula:
Where:
Explanation: The formula accounts for water's slight compressibility under pressure.
Details: Accurate density calculations are crucial for hydraulic systems, deep-sea research, and industrial processes.
Tips: Enter the base density (default 1000 kg/m³), compressibility (default 4.5×10⁻¹⁰ /Pa), and pressure in Pascals. All values must be ≥ 0.
Q1: Why does water density change with pressure?
A: Water is slightly compressible, so increased pressure forces molecules closer together, increasing density.
Q2: What's the typical compressibility of water?
A: Pure water at 20°C has κ ≈ 4.5×10⁻¹⁰ /Pa, but this varies with temperature and purity.
Q3: When would I need to change the base density?
A: For saltwater (≈1025 kg/m³) or at different temperatures (density changes with temperature).
Q4: How significant is pressure's effect on density?
A: At normal pressures, the effect is minimal. Significant changes occur only at very high pressures (e.g., deep ocean).
Q5: Does this account for temperature effects?
A: No, this is an isothermal model. For temperature effects, use a more comprehensive equation of state.