Water Density Formula:
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Definition: This calculator estimates the density of water considering both temperature and pressure effects.
Purpose: It helps engineers, scientists, and students understand how water density changes with environmental conditions.
The calculator uses the formula:
Where:
Explanation: The formula accounts for thermal expansion (temperature effect) and compressibility (pressure effect) on water density.
Details: Accurate water density is crucial for hydraulic systems, oceanography, chemical engineering, and many scientific applications where precise buoyancy or mass calculations are needed.
Tips: Enter the current temperature, pressure, and optionally adjust reference values. Standard conditions are 20°C and 101325 Pa (1 atm).
Q1: How accurate is this calculation?
A: This provides a good approximation for most applications. For extreme conditions, more complex equations may be needed.
Q2: Why does water density change with temperature?
A: Water expands when heated (above 4°C) and contracts when cooled, changing its mass per unit volume.
Q3: How significant is pressure's effect on density?
A: Pressure has minimal effect at low-moderate levels but becomes important in deep ocean or high-pressure systems.
Q4: What's the density of water at 4°C?
A: Pure water reaches maximum density (~999.97 kg/m³) at approximately 4°C at standard pressure.
Q5: Does this work for saltwater?
A: No, seawater requires additional salinity factors in the calculation.