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Temperature Measurement · Free Calculator

Water Density vs Temperature Calculator

Find the density of pure, air free water at a given temperature, for DP level, flow and calibration calculations. The calculator uses the Kell equation, which matches standard tables closely.

Kell equation0 to 150 °CSpecific gravityLevel and flow
°C
Density998.204 kg/m³
Specific gravity (vs water at 4 °C)0.99823
Specific gravity (vs water at 15.56 °C / 60 °F)0.99919
Specific volume1.0018 L/kg
How this result was calculated
  1. ρ(T) = (999.83952 + 16.945176T − 7.9870401×10⁻³T² − 46.170461×10⁻⁶T³ + 105.56302×10⁻⁹T⁴ − 280.54253×10⁻¹²T⁵) ÷ (1 + 16.879850×10⁻³T)
  2. ρ(20 °C) = 998.204 kg/m³

Water density by temperature

°Ckg/m³
0999.84
4999.97
10999.70
15999.10
20998.20
25997.04
30995.65
40992.22
50988.04
60983.20
70977.77
80971.80
90965.32
100958.36
120943.08
150916.83
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Kell Equation (1975)

ρ(T) = (999.83952 + 16.945176T − 7.9870401×10⁻³T² − 46.170461×10⁻⁶T³ + 105.56302×10⁻⁹T⁴ − 280.54253×10⁻¹²T⁵) ÷ (1 + 16.879850×10⁻³T)

T is the temperature in °C and ρ the density in kg/m³ at about 1 atm (saturation pressure above 100 °C). It applies to pure, air free water; dissolved salts or air change the density.

Worked example

Water at 20 °C has a density of 998.20 kg/m³; at 80 °C it is 971.8 kg/m³, about 2.6 % lighter.

Key insight: a DP level transmitter calibrated for cold water reads about 2.6 % high on a hot water tank at 80 °C, because the same level gives less pressure. Calibrate at the operating temperature or compensate.
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Frequently Asked Questions

At what temperature is water densest?

At about 4 °C, where its density is 999.97 kg/m³.

Why does water density matter in instrumentation?

DP level, hydrostatic pressure and mass flow calculations all depend on density, which changes with temperature.

Does pressure change water density?

Only slightly: about 0.05 % per 10 bar. Temperature has a much larger effect.

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