Psychrometric Delta Calculator

Fast deltas for field air condition comparisons. Input two points, choose units, get clear results. Download tables to share with clients and teams easily.

Review these notes before using results:
Enter two air states
Choose a unit system, then supply temperature and relative humidity.
SI (°C, kPa)

Switching units keeps your entered values.
Pressure affects moisture calculations and enthalpy.
Typical sea level: 101.325 kPa.
State 1 Baseline point for deltas.
Dry-bulb temperature of State 1.
Use 0–100%, clamp applied if needed.
Optional label for your records and exports.
State 2 Comparison point after conditioning or mixing.
Dry-bulb temperature of State 2.
Higher RH often increases moisture content.
Optional label for your records and exports.
After calculating, results appear above this form.
Example data table
Use this as a reference for typical air-conditioning changes.
Scenario State 1 State 2 Key expected delta
Cooling + dehumidification 26°C, 55% RH, 101.325 kPa 18°C, 85% RH, 101.325 kPa Δh negative, Δw often decreases
Heating + humidification 18°C, 35% RH, 101.325 kPa 24°C, 45% RH, 101.325 kPa Δh positive, Δw increases
Outdoor-to-indoor mixing 35°C, 60% RH, 101.325 kPa 28°C, 50% RH, 101.325 kPa ΔT drops, ΔRH varies by moisture
Formula used
These equations are standard HVAC approximations for field calculations.
Saturation vapor pressure
Tetens form (kPa), temperature in °C:
Pws = 0.61078 × exp(17.2694×T / (T + 237.3))
Partial vapor pressure
Relative humidity RH in percent:
Pw = (RH/100) × Pws
Humidity ratio
P and Pw in the same pressure units:
w = 0.621945 × Pw / (P − Pw)
Moist air enthalpy
T in °C, h in kJ/kg dry air:
h = 1.006T + w(2501 + 1.86T)
Dew point
Inverse Tetens using Pw (kPa):
Tdp = 237.3 ln(Pw/0.61078) / (17.2694 − ln(Pw/0.61078))
Wet-bulb (approx.)
Stull approximation, Twb in °C:
Twb ≈ f(T, RH)

Deltas: Each delta is calculated as State 2 − State 1 for the same property.
How to use this calculator
  1. Select units matching your instruments and logs.
  2. Set pressure using barometric value or site altitude.
  3. Enter State 1 temperature and relative humidity.
  4. Enter State 2 temperature and relative humidity.
  5. Press Calculate to view properties and deltas above.
  6. Export CSV/PDF to attach to commissioning records.
Tip: Use consistent sensor placement and stabilization time for both states.

Why psychrometric deltas matter on active sites

Construction commissioning often depends on proving a system change, not just a single reading. Delta tracking compares two air states taken at the same barometric pressure, revealing the net effect of cooling, heating, humidification, dehumidification, or mixing. A dry-bulb change of 6°C can occur with minimal moisture change, while a small temperature change may hide a large latent shift.

Inputs that control accuracy

Use calibrated sensors and stable placement. For field checks, keep temperature within −10°C to 50°C when possible, and record relative humidity between 10% and 90% for best sensor performance. Barometric pressure is commonly near 101.3 kPa at sea level and can drop to about 90 kPa around 1,000 m elevation, affecting humidity ratio and enthalpy.

Interpreting humidity ratio and dew point

Humidity ratio (w) reflects actual moisture content, independent of dry-bulb temperature. A reduction from 0.012 to 0.009 kg/kg indicates meaningful drying, even if relative humidity increases due to cooling. Dew point provides a condensation risk indicator; issues become likely when dew point approaches slab, ceiling, or duct temperatures. Many teams flag dew point above 16–18°C as a practical warning during interior finishing.

Using enthalpy delta for load verification

Enthalpy delta summarizes sensible and latent effects in one value. For quick estimates, a −10 kJ/kg change typically signals strong cooling and moisture removal, while +10 kJ/kg often indicates heating and/or humidification. Combine Δh with airflow measurements to compare trends across test steps and to confirm control sequences. When Δw is near zero but ΔT is large, the process is mostly sensible; when Δw drops, latent removal is occurring.

Recommended field workflow and reporting

Capture State 1 at the return or mixed-air location, then capture State 2 at the supply or downstream location after stabilization. Typical comfort supply air may fall near 12–16°C depending on design. Log time, sensor IDs, and pressure method. Exported CSV supports daily QA logs, and the PDF format is convenient for submittals and records.

FAQs

1) What is a psychrometric delta?

It is the difference between two measured air states for the same property, such as ΔT, Δw, or Δh. It highlights the net change caused by equipment, processes, or mixing on site.

2) Why does pressure matter in the results?

Humidity ratio and enthalpy depend on the relationship between vapor pressure and total pressure. Using correct barometric pressure improves moisture calculations, especially at higher elevations.

3) Can relative humidity increase while air is drying?

Yes. Cooling can raise relative humidity even when moisture content falls. Check the humidity ratio (w) and dew point to confirm whether the air is actually gaining or losing moisture.

4) Which delta is best for coil performance checks?

Δh is the most compact indicator because it includes sensible and latent effects. Pair it with airflow or mass flow measurements to compare trends across test steps.

5) How should I take State 1 and State 2 readings?

Use consistent probe depth and location, allow the sensor to stabilize, and record both readings within a short interval. Avoid placing sensors near wet coils, direct sunlight, or leaks.

6) Why is wet-bulb shown as an approximation?

The calculator uses a recognized approximation to provide fast field insight. For high-stakes design verification, confirm wet-bulb using a full psychrometric chart method or certified software.

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Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.