Water Density Equation:
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The water density equation calculates how water density changes with temperature and pressure. It accounts for both compressibility (pressure effects) and thermal expansion (temperature effects) on water density.
The calculator uses the water density equation:
Where:
Explanation: The equation combines the effects of pressure (through the bulk modulus term) and temperature (through the thermal expansion term) on water density.
Details: Accurate water density calculation is crucial for fluid dynamics, oceanography, engineering applications, and scientific experiments where precise density values are needed.
Tips: Enter all values in consistent units (Pa for pressure, K for temperature). Default values are provided for standard conditions (ρ₀=997 kg/m³ at 20°C, P₀=101325 Pa).
Q1: What are typical values for bulk modulus (K)?
A: For water at 20°C, K ≈ 2.15 GPa. It varies slightly with temperature and pressure.
Q2: How does temperature affect water density?
A: Water density decreases with increasing temperature (above 4°C) due to thermal expansion.
Q3: What is the thermal expansion coefficient (β)?
A: For water at 20°C, β ≈ 0.000214 1/K. It increases with temperature.
Q4: Why is reference density important?
A: The reference density (ρ₀) at known conditions (P₀,T₀) serves as the baseline for calculations.
Q5: How accurate is this equation?
A: This provides a good approximation for most applications, but for precise work, consult IAPWS standards.