Psychrometric Chart Calculator

Psychrometric Chart Calculator

Calculate Moist Air Thermodynamic Properties

Calculation Results

Dew Point Temperature °C
Humidity Ratio g/kg dry air
Specific Enthalpy kJ/kg
Vapor Pressure hPa
Specific Volume m³/kg
Saturation Pressure hPa

Understanding the Psychrometric Chart

Psychrometrics is the field of engineering concerned with the physical and thermodynamic properties of gas-vapor mixtures. Most commonly, it refers to the study of moist air (a mixture of dry air and water vapor). A psychrometric chart is a graphical representation of these properties at a constant pressure.

Key Terms Explained

  • Dry Bulb Temperature: The temperature of air measured by a standard thermometer freely exposed to the air but shielded from radiation and moisture.
  • Relative Humidity (RH): The ratio of the current absolute humidity to the highest possible absolute humidity (which depends on the current air temperature).
  • Dew Point: The temperature at which water vapor in the air begins to condense into liquid water (dew).
  • Humidity Ratio (Specific Humidity): The mass of water vapor present in a unit mass of dry air. Usually expressed in grams of water per kilogram of dry air (g/kg).
  • Enthalpy: The total heat content of the moist air, including the sensible heat of the air and the latent heat of the water vapor.

Why Use a Psychrometric Calculator?

While the physical chart is great for visualization, digital calculators provide precision required for HVAC (Heating, Ventilation, and Air Conditioning) design, meteorological analysis, and industrial drying processes. Calculating the dew point is particularly critical for preventing mold growth or condensation on building surfaces.

Example Calculation

If you have an indoor office environment with a Dry Bulb Temperature of 22°C and a Relative Humidity of 50% at standard sea-level pressure (1013.25 hPa):

Property Result
Dew Point 11.12°C
Humidity Ratio 8.28 g/kg
Enthalpy 43.15 kJ/kg

This means that if any surface in the room is colder than 11.12°C, condensation will likely form on that surface.

function calculatePsychrometrics() { var T = parseFloat(document.getElementById("dryBulbTemp").value); var rh = parseFloat(document.getElementById("relHumidity").value); var P = parseFloat(document.getElementById("atmPressure").value); if (isNaN(T) || isNaN(rh) || isNaN(P) || rh 100 || P <= 0) { alert("Please enter valid positive numerical values. Relative humidity must be between 0 and 100."); return; } // Saturation Vapor Pressure (Magnus formula) // es = 6.112 * exp((17.67 * T) / (T + 243.5)) in hPa var es = 6.112 * Math.exp((17.67 * T) / (T + 243.5)); // Actual Vapor Pressure var e = (rh / 100) * es; // Dew Point Temperature // Tdp = (243.5 * ln(e/6.112)) / (17.67 – ln(e/6.112)) var lnE = Math.log(e / 6.112); var Tdp = (243.5 * lnE) / (17.67 – lnE); // Humidity Ratio (w) in kg/kg // w = 0.62198 * e / (P – e) var w = 0.62198 * e / (P – e); var wGrams = w * 1000; // convert to g/kg // Specific Enthalpy (h) in kJ/kg // h = 1.006 * T + w * (2501 + 1.86 * T) var h = 1.006 * T + w * (2501 + 1.86 * T); // Specific Volume (v) in m3/kg // v = Ra * T_kelvin / (P – e) // Ra = 287.058 J/(kg·K) var T_kelvin = T + 273.15; var v = (287.058 * T_kelvin) / ((P – e) * 100); // Update Display document.getElementById("resDewPoint").innerHTML = Tdp.toFixed(2); document.getElementById("resHumRatio").innerHTML = wGrams.toFixed(2); document.getElementById("resEnthalpy").innerHTML = h.toFixed(2); document.getElementById("resVapPress").innerHTML = e.toFixed(2); document.getElementById("resVolume").innerHTML = v.toFixed(3); document.getElementById("resSatPress").innerHTML = es.toFixed(2); document.getElementById("psych-results").style.display = "block"; }

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