What this predictor does
Warm tower exhaust is mixed with ambient air in small steps. At each step, the tool conserves moist-air enthalpy and humidity ratio, then compares the mixed state with the saturation humidity ratio. A visible condensation plume is thermodynamically possible wherever the mixing path lies above saturation.
Inputs
Example conditions
Humidity ratio: W = 0.621945 pv / (P − pv)
Moist-air enthalpy: h = 1.006T + W(2501 + 1.86T) kJ/kg dry air.
For an exhaust dry-air mass fraction x, the model linearly mixes humidity ratio and enthalpy: Wm=(1−x)Wa+xWe and hm=(1−x)ha+xhe. The mixed dry-bulb temperature is recovered from hm and Wm.
Condensation potential is the positive difference Wm−Wsat(Tm). Saturation pressure is evaluated over water above 0°C and over ice below 0°C using Buck-type correlations.
- Ideal adiabatic mixing of two uniform moist-air streams.
- No plume rise, wind field, entrainment rate, droplet-size distribution or aerosol nucleation model.
- The qualitative screening class is not a regulatory or vendor acceptance criterion.
Results
Psychrometric mixing path
The saturation curve is the maximum water-vapour content of air at each temperature. The red portion of the mixing path is above saturation and represents theoretical condensate formation.
Scroll the plot horizontally for readable labels.
How to reduce visible plume
Heating or drying the discharge lowers its relative humidity and can keep the mixing path below saturation.
Plume-abatement systems blend warm dry air with saturated wet-section exhaust before it reaches the atmosphere.
Low ambient temperature and high relative humidity are typically the most plume-prone combination. Use site weather bins, not annual averages.
For roads, airports, buildings or electrical equipment, use a site-specific dispersion/CFD study that addresses plume rise, recirculation, icing and ground contact.
Interpretation and limitations
The predictor answers one question only: can ideal mixing cause supersaturation? A positive result does not mean a long or ground-level plume will occur. Wind speed, turbulence, exit velocity, tower geometry, ambient stability, droplet nuclei and sunlight all affect observed visibility.
- EnergyPlus Psychrometric Services documentation: moist-air humidity ratio, enthalpy, saturation pressure and related state functions.
- US EPA cooling-tower plume studies: visible wet-tower plumes are primarily condensed water vapour; cold, humid conditions increase plume potential.
- Use project specifications, tower-vendor performance data and site meteorology for design decisions.