Results
| T (°C) | ρ (kg/m³) | μ (Pa·s) | ν (m²/s) | β (1/K) |
|---|---|---|---|---|
| No results yet. Click Calculate or try the example below. | ||||
Example data (0, 20, 40, 60, 80, 100 °C)
| T (°C) | ρ (kg/m³) | μ (Pa·s) | ν (m²/s) | β (1/K) |
|---|
Formulas used
Assumptions: Pure water at approximately atmospheric pressure, temperature 0–100 °C.
- Density, ρ (kg/m³)
Empirical fit (widely cited approximation):
ρ(T) = 1000 · [1 − ((T + 288.9414) / (508929.2 · (T + 68.12963))) · (T − 3.9863)²]
whereTis in °C. - Dynamic viscosity, μ (Pa·s)
Andrade-type correlation for water in 0–100 °C:
μ(T) = 2.414×10⁻⁵ · 10^( 247.8 / (T + 133.15) )withTin °C. - Kinematic viscosity, ν (m²/s)
ν(T) = μ(T) / ρ(T) - Volumetric thermal expansion coefficient, β (1/K)
Defined at constant pressure:β = −(1/ρ) · (dρ/dT). We computedρ/dTvia a symmetric finite difference.
Correlations provide engineering accuracy for common temperatures. For ultra‑precise metrology, consult primary reference data.
How to use this calculator
- Select Single temperature or Range.
- Enter temperature in °C. For ranges, provide start, end, and step.
- Click Calculate to populate the results table.
- Optionally click Download CSV or Download PDF to export.
- Use the Example data card to preview typical values quickly.
- Keep temperatures within 0–100 °C for the most reliable outputs.