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Water Activity from Equilibrium Relative Humidity

Convert equilibrium relative humidity (ERH) to water activity (a_w) with optional temperature correction for hygroscopic systems.

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1. Define Input Parameters

2. Engineering Output

Maximum ERH (ERH_max)
- %RH
Temperature difference (delta_T)
- °C
Corrected ERH (ERH_corr)
- %RH
Water activity (a_w)
- dimensionless

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Context & Assumptions

Water activity quantifies free water availability and drives microbial growth and chemical stability. This calculator converts measured ERH to a_w and applies a linear temperature correction when storage conditions differ from the reference temperature.

Understand the Engineering Principles

Review the step-by-step derivations, typical industrial limits, and scale-up rules.

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