Abstract
The water activity (aw) of eight salt solutions was determined at three temperatures (25, 30, 45°C) using a pressure transducer‐vapor pressure manometer. The aws of the salts showed a decrease with increasing temperature, which was explained with the help of a thermodynamic equation. This is opposite to the increase in aw with increase in temperature for foods. Moisture sorption data for fish flour and cornmeal were obtained at 25–65°C. The Guggenheim‐Anderson‐deBoer model was evaluated and shown to be comparable to the Brunauer‐Emmett‐Teller model for prediction of the monolayer. Product was equilibrated at different aws at 25°C then subsequently shifted to 30°C and 45°C in a sealed chamber. The resultant a, change, measured on the Kaymont‐Rotronics, was predictable from the isotherm at each temperature using the Clausius Clapeyron relationship.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 385-392 |
| Number of pages | 8 |
| Journal | Journal of food science |
| Volume | 50 |
| Issue number | 2 |
| DOIs | |
| State | Published - Mar 1985 |
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