Density at state

Moist-air density calculator

Calculate moist-air and dry-air density from temperature, humidity and pressure with explicit basis and units.

Reviewed
2 September 2026
Verified calculation core pw-core 0.1
01

Known properties

Define state A

Enter measured pressure when available. Sea-level standard is 101.325 kPa.

02

Pressure-aware plot

State geometry

Pressure-aware psychrometric chartDry-bulb temperature against humidity ratio with relative-humidity curves and 1 labeled moist-air state.01020304050051015202530ADry-bulb temperature (°C)Humidity ratio (g/kg dry air)100% RH
Chart data alternative

Scroll horizontally to see every column.

StateDry bulbHumidity ratioRHPressure
A25.00 °C9.883 g/kg50.0%101.325 kPa

01

Best input pair and density basis

Dry bulb plus humidity ratio is useful when a moisture balance already provides W; dry bulb plus RH is more common for direct probes. Enter actual station pressure when converting measured volume flow to mass flow.

Dry-air density is the reciprocal of specific volume on a dry-air mass basis. Moist-air density includes vapor mass in the same mixture volume. State which basis is used rather than labeling both simply air density.

02

Verified example

At 25 °C, 50% RH and 101.325 kPa, moist-air density is 1.1770 kg/m³ and specific volume is 0.858 m³/kg dry air. At 84.6 kPa, moist-air density falls to 0.9815 kg/m³ and specific volume rises to 1.031 m³/kg dry air.

A nominal 1 m³/s stream therefore does not carry the same mass at those pressures. Use the density corresponding to the measured state and the definition expected by the fan or balance calculation.

03

Interpretation for field work

Temperature and pressure usually dominate density; moisture has a smaller real effect because water vapor has lower molecular mass than dry air. Record whether the volume flow is actual or standardized before multiplying.

For commissioning, keep density conversion separate from sensor accuracy and duct traverse quality. A precise psychrometric calculation cannot rescue an unrepresentative velocity profile.

04

Common mistakes

Do not use gauge pressure, airport altimeter setting without understanding its reduction, or elevation as if it were measured pressure. Do not invert moist-air density and call the result dry-air-basis specific volume without converting the basis.

Avoid mixing standard cubic units with actual cubic units. Round only after completing the mass-flow calculation, especially when comparing two branches.

05

Limits and connected workflow

The perfect-gas model is intended for the documented atmospheric temperature and pressure range; non-ideal high-pressure effects are excluded. Critical metering requires the instrument and contractual density convention.

Use the altitude reference for a correction sequence, then the HVAC commissioning page to connect corrected mass flow with outdoor, return and supply states.