Mixed Air Calculator

Calculate mixed air temperature, relative humidity, humidity ratio, enthalpy, dew point, and airflow based on two air-stream flow rates, temperatures, relative humidities, and barometric pressure. Mixed Air Calculator helps HVAC engineers, designers, technicians, and building operators evaluate ventilation and conditioning performance.

Highlights

  • Calculates mixed-air temperature from outdoor and return air streams.
  • Determines mixed-air relative humidity, humidity ratio, and dew point.
  • Computes mixed-air enthalpy for HVAC heating and cooling analysis.
  • Supports multiple airflow, temperature, pressure, and energy units.
  • Ideal for HVAC engineers, technicians, designers, and building operators.

Table of Contents

  1. How Mixed Air Calculator Works?
  2. Practical Use Cases
  3. Accuracy and Limitations
  4. Quick Examples
  5. Frequently Asked Questions (FAQs)
  6. Cite This Calculator

How Mixed Air Calculator Works?

The Mixed Air Calculator applies steady-state psychrometric mass and energy balances to combine outdoor air and return air. It uses the outdoor airflow, return airflow, dry-bulb temperatures, relative humidities, and barometric pressure to determine the condition of the resulting air stream.

For each air stream, saturation vapor pressure is determined from temperature. The water-vapor partial pressure is then calculated from relative humidity:

Pv=φPsat(T)

Here, φ is relative humidity expressed as a fraction, Psat is saturation pressure, and Pv is vapor partial pressure. Humidity ratio, defined as the mass of water vapor per mass of dry air, is calculated by:

W=0.621945PvP-Pv

where P is barometric pressure. The dry-air density associated with each stream can be estimated using the ideal-gas relationship:

ρda=P-PvRdaT

The dry-air mass flow for each inlet is obtained by multiplying dry-air density by volumetric airflow. The combined dry-air mass flow is:

m˙da,mix=m˙da,o+m˙da,r

Moisture is conserved during adiabatic mixing, so the mixed humidity ratio is the dry-air-mass-weighted average of the two inlet humidity ratios. Enthalpy is balanced in the same way:

Wmix=m˙da,oWo+m˙da,rWrm˙da,mix
hmix=m˙da,oho+m˙da,rhrm˙da,mix

For ordinary HVAC psychrometric calculations, moist-air enthalpy is approximated by:

h=1.006T+W(2501+1.86T)

The mixed dry-bulb temperature is recovered from mixed enthalpy and humidity ratio:

Tmix=hmix-2501Wmix1.006+1.86Wmix

Finally, the mixed vapor pressure is obtained from the mixed humidity ratio, and it is used with the mixed saturation pressure to calculate relative humidity. Dew point is the temperature at which the mixed vapor pressure equals saturation pressure. Mixed airflow is calculated from the mixed moist-air density and the combined dry-air mass flow.


Calculated resultPrimary basis
Mixed AirflowCombined dry-air mass flow and mixed moist-air density
Mixed Dry-Air Mass FlowOutdoor and return dry-air mass-flow sum
Mixed Air TemperatureEnthalpy and moisture balance
Mixed Relative HumidityMixed vapor pressure compared with saturation pressure
Mixed Humidity RatioDry-air-mass-weighted moisture balance
Mixed EnthalpyDry-air-mass-weighted energy balance
Mixed Dew PointTemperature corresponding to mixed vapor pressure

Practical Use Cases

HVAC engineers can use the calculator to estimate the entering-air condition at an air-handling unit when outdoor ventilation air combines with return air. The results support coil-load calculations, equipment selection, and evaluation of heating or cooling requirements.

Building designers can assess how different outdoor-air and return-air proportions affect mixed temperature, humidity ratio, enthalpy, and dew point during design conditions.

HVAC technicians can compare measured outdoor and return conditions with expected mixed-air properties when troubleshooting dampers, mixing boxes, economizer operation, or abnormal coil performance.

Building operators can evaluate ventilation strategies by observing how changes in outdoor airflow influence indoor air-conditioning demand and mixed-air humidity.

Energy analysts can use mixed-air enthalpy and dry-air mass flow to estimate the sensible and latent conditioning burden imposed on heating and cooling equipment.

Industrial and process-air users can examine the combined moisture and temperature condition before air enters a drying, storage, manufacturing, or environmental-control process.

Accuracy and Limitations

The calculator is suitable for steady-state HVAC mixing estimates when outdoor and return streams are well mixed, pressure is uniform, and no moisture condenses or evaporates during mixing. Its results depend on the accuracy of the entered airflow, temperature, relative humidity, and barometric pressure; relative-humidity errors can substantially affect humidity ratio and dew point, especially near saturation. The psychrometric relationships use ideal-gas behavior and standard moist-air enthalpy approximations, so results may differ slightly from detailed psychrometric software. The calculation does not model duct heat transfer, fan heat, damper leakage, stratification, coil contact effects, condensation, or transient changes.

Quick Examples

Example #1: Cold Winter Ventilation

Evaluate mixed-air conditions when cold, humid outdoor air combines with warm return air in a commercial HVAC system.

Example #2: Hot Summer Air Mixing

Assess the psychrometric condition of mixed air during summer operation with hot outdoor air and conditioned return air.

Example #3: High-Elevation Building

Calculate mixed-air properties for a building at elevation using reduced atmospheric pressure and airflow values in cubic meters per hour.

Frequently Asked Questions

Mixed air is the combined stream formed when outdoor air blends with return air from a conditioned space. Its temperature and moisture properties depend on the conditions and proportions of both streams.

Outdoor air can raise or lower the mixed-air temperature and change its moisture content. The effect is greater when the outdoor-air portion of the total airflow increases.

Atmospheric pressure affects air density, humidity ratio, dew point, and enthalpy. Local pressure is especially important at elevations significantly above or below sea level.

Mixed-air dew point is the temperature at which water vapor begins to condense. It helps identify potential condensation risks on cooling coils, ducts, windows, and other cold surfaces.

Relative humidity depends on both moisture content and temperature. Even when no moisture is added or removed, blending warmer and cooler air can significantly change the resulting relative humidity.

Cite This Calculator