Air Mixing (Psychrometric)

Mix two moist-air streams (such as outdoor air and return air) into a single mixed-air condition. Returns the mass-weighted mixed dry-bulb, humidity ratio, enthalpy, relative humidity and dew point, with a per-stream enthalpy chart.


ASHRAE Fundamentals · Psychrometric Mixing

Flow Basis

Pa

Stream 1 (e.g. outdoor air)

kg/s
°C
%

Stream 2 (e.g. return air)

kg/s
°C
%

Mixed Air

26.75°C
Dry-bulb T
47.9%
Rel. humidity
10.48g/kg
Humidity ratio
53.67kJ/kg
Enthalpy
14.8°C
Dew point
4.000kg/s
Total dry-air flow

Enthalpy by Stream

Stream 1Stream 2Mixed020406080h (kJ/kg)

About Air Mixing Calculator (Psychrometric)

The air mixing calculator finds the condition of the single air stream produced when two moist-air streams combine adiabatically, the classic case being outdoor (fresh) air mixing with recirculated return air before it enters a cooling or heating coil. On a dry-air mass basis the mixed dry-bulb temperature, humidity ratio, and enthalpy are each the mass-weighted average of the two inlet streams.

Enter each stream's flow rate, dry-bulb temperature, and relative humidity, plus the atmospheric pressure. The tool computes each stream's humidity ratio and enthalpy from the Magnus saturation-pressure relation (the same form used in the psychrometric calculator), weights them by dry-air mass flow, and reports the mixed dry-bulb, humidity ratio, enthalpy, dew point, and a relative humidity back-calculated from the mixed condition. Flows may be entered as dry-air mass flow or as volumetric flow, which is converted to mass flow using each stream's moist-air density.

How It Works

  1. Enter the flow, dry-bulb temperature, and relative humidity of both streams and the atmospheric pressure; choose a mass or volumetric flow basis.
  2. For each stream the tool finds the saturation pressure Pws (Magnus), the vapour pressure Pw = RH·Pws, the humidity ratio W = 0.62198·Pw/(P−Pw), and the enthalpy h = 1.006·T + W·(2501 + 1.86·T).
  3. Volumetric flows are converted to dry-air mass flow with the specific volume v = Rda·(T+273.15)·(1+1.6078·W)/P, so the weighting is always on a dry-air basis.
  4. The mixed condition is the mass-weighted average: T_m, W_m, and h_m. The mixed RH and dew point are back-calculated from W_m and T_m (capped at saturation).

Worked Example

A unit mixes 1 kg/s of outdoor air at 35 °C, 40% RH with 3 kg/s of return air at 24 °C, 50% RH at 101.325 kPa. The dry-bulb mixes as T_m = (1×35 + 3×24)/4 = 26.75 °C. The stream humidity ratios are W₁ ≈ 14.11 g/kg and W₂ ≈ 9.28 g/kg, giving W_m = (1×14.11 + 3×9.28)/4 ≈ 10.48 g/kg. The enthalpies are h₁ ≈ 71.41 and h₂ ≈ 47.76 kJ/kg, so h_m = (1×71.41 + 3×47.76)/4 ≈ 53.67 kJ/kg. Back-calculating from W_m at 26.75 °C gives a mixed relative humidity of about 47.9% and a dew point near 14.8 °C.

Formulas

Mixed dry-bulb temperature
T_m = (m1*T1 + m2*T2) / (m1 + m2)
Mixed humidity ratio (mass balance)
W_m = (m1*W1 + m2*W2) / (m1 + m2)
Mixed enthalpy (energy balance)
h_m = (m1*h1 + m2*h2) / (m1 + m2)
Stream humidity & enthalpy (Magnus)
Pws = 610.94*exp(17.625*T/(T+243.04)); W = 0.62198*Pw/(P-Pw); h = 1.006*T + W*(2501 + 1.86*T)
Volume-to-mass conversion
m_dot = V_dot / v , v = Rda*(T+273.15)*(1 + 1.6078*W)/P

Standards & References

  • ASHRAE Handbook — Fundamentals, "Psychrometrics" (adiabatic mixing of two airstreams)
  • ASHRAE Standard 62.1 (outdoor-air/return-air mixing for ventilation)
  • Magnus-Tetens saturation form (Alduchov & Eskridge)
  • Conservation of dry-air mass, water mass, and energy

Frequently Asked Questions

Why is the mixing weighted by mass and not by volume?

Mass of dry air, water vapour, and energy are conserved on mixing; volume is not, because density changes with temperature. The tool therefore weights by dry-air mass flow. If you enter volumetric flows it first converts each to mass flow using the stream's specific volume.

Why does the mixed temperature sit closer to the larger stream?

The mixed dry-bulb is the mass-weighted average T_m = (m1·T1 + m2·T2)/(m1+m2). A stream carrying more mass dominates the average, so a 75% return-air / 25% outdoor-air mix lands near the return-air temperature.

Can the mixed air be saturated or foggy?

Yes. Mixing two streams that are each near saturation can produce a point above the saturation line on the psychrometric chart, implying fog. The calculator caps the reported relative humidity at 100% and the dew point at the mixed dry-bulb when that happens.

Which saturation formula does the tool use?

It uses the Magnus-Tetens form Pws = 610.94·exp(17.625·T/(T+243.04)) Pa, the same relation as the psychrometric calculator, so humidity ratios and enthalpies are consistent between the two tools to within a few tenths of a percent of the ASHRAE tables.