Moisture reference · air is only one part

Psychrometrics for drying and storage

Use humidity ratio, dew point and temperature together when evaluating drying potential and storage condensation risk.

Reviewed
2 September 2026

Original field diagram

Air, surface and material

Air statetemperature · RH · humidity ratio · dew point
Coldest surfaceCompare surface temperature with dew point plus an uncertainty margin
Material criterionApply product-specific moisture, time and acceptance limits
Use dew point for the coldest-surface comparison and humidity ratio for air-side moisture transfer. Apply a separate material-specific acceptance criterion.

01

Separate air condition from material condition

Air psychrometrics describes the gas state. Drying rate also depends on material moisture, surface area, airflow, transfer resistance and time. Storage risk also depends on product and enclosure surface temperatures.

Use the calculator to establish the air-side moisture potential, then apply material-specific limits and measurement practice.

02

Verified air-state examples

At 30 °C/40% RH/101.325 kPa, air contains 10.604 g/kg, has a 14.936 °C dew point and 57.293 kJ/kg enthalpy. At 20 °C/60% RH, it contains 8.736 g/kg with a 12.008 °C dew point.

The warmer air has lower RH yet more water per kg dry air. This is why RH alone cannot rank moisture load across temperatures.

03

Assess condensation risk

Compare dew point with the coldest plausible product, wall, pipe or package surface. At 5 °C/80% RH, dew point is 1.842 °C and humidity ratio is 4.314 g/kg. Moving that air into a warmer space changes RH but not its moisture coordinate unless water transfers.

Use an uncertainty margin and account for thermal bridges, door openings and overnight transients. A room-average probe cannot guarantee every surface is safe.

04

Assess drying direction

Compare inlet and exhaust humidity ratio. Rising exhaust W supports moisture pickup when airflow and sampling are representative. Multiply delta W by verified dry-air mass flow to estimate a water rate, keeping units and time basis explicit.

Do not infer product dryness from air equilibrium alone. Hygroscopic materials require sorption data and an acceptance method appropriate to the product.

05

Limits and next action

The model excludes liquid films, adsorption, biological growth and transient heat/mass transfer. It cannot set a universal safe RH or storage duration.

Next action: calculate inlet and exhaust states at measured pressure, compare humidity ratio and dew point, then document the material-specific criterion used for the actual decision.