Viscosity of water

Chemcasts Team
October 28, 2025
Understand the viscosity of water — its definition, types, empirical equations, and variation with temperature and pressure. Includes engineering significance and data for process applications.

Understanding the Viscosity of Water – A Key Property for Process Engineers

Water is the lifeblood of nearly every chemical and process plant. It serves as a solvent, coolant, heat-transfer medium, cleaning agent, and transport fluid. Despite its ubiquity, one of its most critical physical properties—viscosity—is frequently misunderstood or oversimplified in early design stages. Misjudging viscosity leads to undersized pumps, inaccurate flow meters, poor mixing, excessive pressure drops, and even operational failures. This comprehensive post explores the fundamentals of water viscosity, its strong temperature dependence, practical calculation methods with step-by-step examples, measurement techniques, and real-world engineering implications.


What Is Viscosity? A Closer Look

Dynamic viscosity (μ), also called absolute viscosity, measures a fluid’s internal resistance to shear stress. It quantifies how “thick” or “sticky” a fluid is. For water, values are reported in Pas\mathrm{Pa \cdot s} (Pascal-seconds) or more commonly mPas\mathrm{mPa \cdot s} (millipascal-seconds), where 1mPas=1cP1 \, \mathrm{mPa \cdot s} = 1 \, \mathrm{cP} (centipoise).

Kinematic viscosity (ν) is defined as:

ν=μρ\nu = \frac{\mu}{\rho}

where ρ\rho is fluid density (kg/m³). Kinematic viscosity is preferred in gravity-driven flows (e.g., open channels, tank draining) and in the Reynolds number calculation:

Re=ρvDμ=vDν\mathrm{Re} = \frac{\rho v D}{\mu} = \frac{v D}{\nu}

For pure water at 20 °C and 1 atm:

  • μ1.002mPas\mu \approx 1.002 \, \mathrm{mPa \cdot s} (1.002 cP)
  • ρ998.2kg/m3\rho \approx 998.2 \, \mathrm{kg/m^3}
  • ν1.004mm2/s\nu \approx 1.004 \, \mathrm{mm^2/s} (1.004 cSt)

Note: Water is a Newtonian fluid—its viscosity is independent of shear rate under normal process conditions.


Temperature Dependence: The Dominant Factor

Water’s viscosity decreases exponentially with increasing temperature. This behavior arises from weakened hydrogen bonding at higher kinetic energies.

Below is a high-accuracy table based on the IAPWS-95 formulation (values rounded to three decimals):

Temp (°C)μ (mPa·s)ρ (kg/m³)ν (mm²/s)
01.787999.81.787
51.519999.91.519
101.307999.71.307
151.139999.11.140
201.002998.21.004
250.890997.00.893
300.798995.70.802
350.719994.00.724
400.653992.20.658
450.596990.20.602
500.547988.00.554
550.504985.70.511
600.467983.20.475
650.434980.60.443
700.404977.80.413
750.378974.90.388
800.355971.80.365
850.334968.60.345
900.315965.30.326
950.298961.90.310
1000.282958.40.294

Plotting tip: Plot ln(μ)\ln(\mu) vs. 1T+273.15\frac{1}{T + 273.15} to get a near-linear trend for interpolation in Excel or Python.


Accurate Calculation Formula (10–100 °C, ±0.8 %)

The Vogel-type equation is widely used:

μ(T)=2.414×105×10247.8T+133.15\mu(T) = 2.414 \times 10^{-5} \times 10^{\frac{247.8}{T + 133.15}}

  • TT = temperature in °C
  • μ\mu = dynamic viscosity in Pas\mathrm{Pa \cdot s}
  • Multiply by 1,000mPas\mathrm{mPa \cdot s}

This equation fits IAPWS data extremely well across typical process ranges.


Pressure Effects: When Do They Matter?

At standard pressures (< 50 bar), viscosity changes by less than 1 %—negligible for most applications.

However, in:

  • High-pressure boilers (> 100 bar)
  • Deep-well injection
  • Subsea pipelines

viscosity increases slightly. A rule of thumb: +0.2 % per 10 bar above 1 atm.

For precision work, use the IAPWS-2008 correlation for high-pressure water properties.


Measuring Viscosity: Lab and Plant Methods

Accurate measurement requires temperature control to ±0.1 °C.

MethodBest ForAccuracyCost
Capillary (Ostwald)Lab, pure fluids±0.1 %Low
Rotational (Brookfield)QC, slurries±1 %Medium
Vibrating probeInline process monitoring±1–2 %High
Falling ballEducation, demos±2–5 %Low

Pro tip: Always calibrate with certified viscosity standards (e.g., Cannon Instrument Co.).


Why Viscosity Matters in Process Design

1. Pump Selection & NPSH

Higher μ\mu → higher frictional losses in suction lines → increased NPSHr.
Cold water at 5 °C has ~70 % higher viscosity than at 30 °C → risk of cavitation in winter.

2. Pipe Sizing & Pressure Drop

Use Darcy-Weisbach equation:

ΔP=fLDρv22\Delta P = f \frac{L}{D} \frac{\rho v^2}{2}

where ff depends on Re, which depends on ν\nu.
Undersized lines in cold climatesexcessive ΔPpump overload.

3. Mixing and Agitation

In laminar regime (Re < 2,300), power scales with μ\mu.
Cold, viscous water requires higher impeller speeds or larger motors.

4. Heat Transfer

Nusselt number correlations (e.g., Dittus-Boelter) depend on Re and Pr:

Pr=cpμk\mathrm{Pr} = \frac{c_p \mu}{k}

Higher μ\mu → higher Pr → thicker thermal boundary layerlower h.

5. Filtration and Membranes

Cake resistance ∝ μ\mu.
Winter drop from 25 °C to 5 °C~70 % flux reduction if not heated.


Viscosity Calculation Examples (Step-by-Step)

Example 1: Calculate μ at 37 °C using the formula

μ(37)=2.414×105×10247.837+133.15\mu(37) = 2.414 \times 10^{-5} \times 10^{\frac{247.8}{37 + 133.15}}

  1. T+133.15=170.15T + 133.15 = 170.15
  2. 247.8170.151.456\frac{247.8}{170.15} \approx 1.456
  3. 101.45628.5110^{1.456} \approx 28.51
  4. μ=2.414×105×28.516.88×104Pas\mu = 2.414 \times 10^{-5} \times 28.51 \approx 6.88 \times 10^{-4} \, \mathrm{Pa \cdot s}
  5. μ=0.688mPas\mu = 0.688 \, \mathrm{mPa \cdot s}

Table check (interpolated):
35 °C = 0.719, 40 °C = 0.653 → 37 °C ≈ 0.690 mPa·s
Error: < 0.3 %


Example 2: Kinematic viscosity at 72 °C for pipeline design

From table:

  • μ0.391mPas\mu \approx 0.391 \, \mathrm{mPa \cdot s} (avg. 70 & 75 °C)
  • ρ976.4kg/m3\rho \approx 976.4 \, \mathrm{kg/m^3}

ν=0.391×103976.4=4.00×107m2/s=0.400mm2/s\nu = \frac{0.391 \times 10^{-3}}{976.4} = 4.00 \times 10^{-7} \, \mathrm{m^2/s} = 0.400 \, \mathrm{mm^2/s}

Reynolds number (DN100 pipe, v = 2 m/s):
Re=vDν=2×0.10.0004×103=500,000(turbulent)\mathrm{Re} = \frac{v D}{\nu} = \frac{2 \times 0.1}{0.0004 \times 10^{-3}} = 500,000 \quad (\text{turbulent})


Example 3: Cooling water viscosity drop in winter

Summer: 28 °C → μ0.84mPas\mu \approx 0.84 \, \mathrm{mPa \cdot s}
Winter: 6 °C → interpolate:
μ1.47mPas\mu \approx 1.47 \, \mathrm{mPa \cdot s} (75 % higher)

Impact on centrifugal pump:

  • ΔPμ\Delta P \propto \mu75 % higher head loss
  • Power ∝ ΔP×Q\Delta P \times Q~50–60 % higher power
  • Risk: Motor trip or reduced flow

Solution:

  • Install suction line heater
  • Use VFD to boost speed
  • Accept lower flow in winter

Example 4: Heat exchanger design check

Water enters at 15 °C, exits at 45 °C. Use average μ.

  • μ151.139mPas\mu_{15} \approx 1.139 \, \mathrm{mPa \cdot s}
  • μ450.596mPas\mu_{45} \approx 0.596 \, \mathrm{mPa \cdot s}
  • Average μ0.868mPas\mu \approx 0.868 \, \mathrm{mPa \cdot s}

Use this in LMTD correction and Re calculations for accurate U-value.


Takeaway

Water viscosity is not constant. A 20 °C temperature change can alter μ\mu by over 100 %. Always:

  • Use temperature-specific values
  • Include margin in cold-weather design
  • Validate with lab measurements
  • Document reference conditions

Armed with the table, formula, and examples above, you can now confidently size equipment, troubleshoot flow issues, and optimize processes year-round.