Dynamic Viscosity of Water at 20 °C

μw=0.001002 Pa⋅s\mu_{w} = 0.001002\ \text{Pa}{\cdot}\text{s}
Value0.001002 Pa·s
StatusMeasured: ± 0.000005 Pa·s (0.005 relative)
SourceIAPWS / CRC Handbook of Chemistry and Physics, 104th ed.
CategoriesMaterial PropertiesEngineering & TradeFluid Properties
Dynamic Viscosity of Water at 20 °C in every dynamic viscosity unit
micropascal second1,002 μPa·s
millipoise10.02 mP
pound per foot hour2.4239265 lb/(ft·h)
millipascal second1.002 mPa·s
centipoise1.002 cP
microreyn0.14532781 μreyn
poise0.01002 P
pascal second0.001002 Pa·s
pound per foot second0.00067331291 lb/(ft·s)
pound-force second per square foot0.000020927205 lbf·s/ft²
kilopascal second0.000001002 kPa·s
reyn1.4532781e-07 reyn

Learning zone

Water at 20 °C is very nearly exactly 1 centipoise, which is not a coincidence: the poise scale was set up so that water would land there. The kinematic viscosity is 1.004 × 10⁻⁶ m²/s, or 1.004 centistokes. Both feed the Reynolds number, and therefore every friction factor, settling velocity and pump-suction calculation you will do with water.

Temperature dominates, and by more than most people expect. Water at 5 °C is 1.52 mPa·s and at 80 °C only 0.355 — a factor of four across ordinary building temperatures. Since Re scales as 1/µ, a chilled-water line and a heating line at the same velocity are at very different Reynolds numbers, and laminar-regime behaviour in cold, small-bore or glycol-laden lines is far more common than designers assume. Pressure barely matters for liquids. Add 50 % propylene glycol and viscosity at 0 °C rises to roughly 15 mPa·s, at which point coil film coefficients collapse and pump curves stop matching the catalogue.