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Fluid mechanics / Describe the flow

FLUID MECHANICS · 01–02 / BASIC

Density, pressure & viscosity

Definitions, SI units, validity conditions and a worked water-property example for density, pressure and viscosity in fluid mechanics.

9 min read2026-08-13Definitions, equations & units checkedJA version

Abstract

Density measures mass per unit volume, pressure is the isotropic normal stress in a fluid at rest, and viscosity quantifies resistance to the rate of deformation. Together they characterize inertia, mechanical state and momentum transport.

ρ = m / Vp = Fₙ / Aτ = μ du/dy
02.

Density: connecting mass and volume

For a uniform sample, mean density ρ is mass m divided by volume V. Continuum mechanics uses a local field ρ(x, t), defined over a sampling volume that is small macroscopically but still large relative to molecular scales.

Liquid density is often treated as constant over ordinary pressure ranges. Gas flows, high-speed flows and problems with large temperature differences generally require density to vary with pressure and temperature.

Equation (1)Mean density
ρ=mV\rho=\frac{m}{V}
ρ\rho
Density[kg/m3\mathrm{kg/m^3}]
mm
Mass[kg\mathrm{kg}]
VV
Volume[m3\mathrm{m^3}]
Physical role
Appears in mass conservation and inertia; it fixes how much matter occupies a given volume.
State dependence
Generally depends on temperature and pressure and may change abruptly across a phase boundary.
03.

Pressure: stress normal to a surface

In a fluid at rest, the stress acting across any plane through a point is normal to that plane and independent of its orientation. Its magnitude is pressure p. When the stress is nearly uniform over a finite area, it can be evaluated as normal force Fₙ divided by area A. The pascal is defined by 1 Pa = 1 N/m² [1].

Absolute pressure uses perfect vacuum as its zero; gauge pressure uses the surrounding atmospheric pressure. Equations of state and comparisons with vapor pressure normally require absolute pressure.

Equation (2)Uniform normal stress
p=FnAp=\frac{F_{\mathrm n}}{A}
pp
Pressure[Pa\mathrm{Pa}]
FnF_{\mathrm n}
Normal force[N\mathrm{N}]
AA
Loaded area[m2\mathrm{m^2}]
Equation (3)Absolute and gauge pressure
pabs=pgauge+patmp_{\mathrm{abs}}=p_{\mathrm{gauge}}+p_{\mathrm{atm}}
pabsp_{\mathrm{abs}}
Absolute pressure[Pa\mathrm{Pa}]
pgaugep_{\mathrm{gauge}}
Gauge pressure[Pa\mathrm{Pa}]
patmp_{\mathrm{atm}}
Ambient atmospheric pressure[Pa\mathrm{Pa}]
04.

Viscosity: transport of momentum across velocity gradients

Consider simple shear, u = u(y). In a Newtonian fluid, shear stress τ is proportional to shear rate du/dy; the coefficient μ is the dynamic viscosity, not the kinematic viscosity [2, 3].

Kinematic viscosity ν is μ divided by density ρ and is useful when comparing viscous momentum diffusion with inertia. Both μ and ν depend on temperature; for liquids, μ generally decreases as temperature rises.

Equation (4)Newton's law of viscosity
τ=μdudy\tau=\mu\frac{\mathrm d u}{\mathrm d y}
Newtonian fluid in simple shear
τ\tau
Shear stress[Pa\mathrm{Pa}]
μ\mu
Dynamic viscosity[Pa⋅s\mathrm{Pa{\cdot}s}]
du/dy\mathrm d u/\mathrm d y
Shear rate[s−1\mathrm{s^{-1}}]
Equation (5)Kinematic viscosity
ν=μρ\nu=\frac{\mu}{\rho}
ν\nu
Kinematic viscosity[m2/s\mathrm{m^2/s}]
μ\mu
Dynamic viscosity[Pa⋅s\mathrm{Pa{\cdot}s}]
ρ\rho
Density[kg/m3\mathrm{kg/m^3}]
Newtonian fluid
Stress and shear rate are linearly related, so μ can be treated as a state-dependent material property.
Non-Newtonian fluid
Paints, slurries and polymer solutions may have an apparent viscosity that depends on shear rate or flow history.
05.

Worked example: kinematic viscosity of water at 20 °C

For water near 0.1 MPa and 20 °C, use the representative rounded values ρ = 998.2 kg/m³ and μ = 1.002 × 10⁻³ Pa·s. These values are consistent with the IAPWS-based reference correlations described by NIST; precision work should evaluate the standard formulations at a stated temperature and pressure [4, 5].

Substitution in Equation (5) gives ν = (1.002 × 10⁻³) / 998.2 ≈ 1.004 × 10⁻⁶ m²/s. A property-table value should always be reported with temperature, pressure, units and appropriate significant figures.

Illustrative water properties near 20 °C
QuantitySymbolValueSI unit
Densityρ998.2kg/m³
Dynamic viscosityμ1.002 × 10⁻³Pa·s
Kinematic viscosityν1.004 × 10⁻⁶m²/s

References