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OSMO-CONVECTIVE DRYING OF GRAPES
Authors:S Grabowski  AS Mujumdar  HS Ramaswamy  C Strumillo
Affiliation:1. Department of Food Science , Macdonald Campus of McGill University , Ste Anne de Bellevue, Quebec, H9X 3V9, Canada;2. Faculty of Process and Environmental Engineering, Lodz Technical University , ul. Wolczanska 175, Lodz, 90-924, Poland;3. Department of Chemical Engineering , McGill University , Montreal, PQ, H3A 2A7, Canada;4. Department of Food Science , Macdonald Campus of McGill University , Ste Anne de Bellevue, Quebec, H9X 3V9, Canada;5. Faculty of Process and Environmental Engineering, Lodz Technical University , ul. Wolczanska 175, Lodz, 90-924, Poland
Abstract:ABSTRACT

In order to reduce browning of grapes during drying, a special drying method was developed and evaluated using a laboratory scale fluidized bed dryer. Fresh Thompson seedless grapes were initially dried by immersion in a fluidized bed of sugar. The mass ratio of grapes to sugar was 1:1. The flow rate of hot air (at 45 and 60°C) was sufficient to fluidize the sugar bed, while grapes placed on the screen, 3 cm above the drying air distributor, remained generally stationary.

Due to the simultaneous osmotic and convection drying effects, the drying time was reduced by factor ~1.5 as compared to drying under the similar conditions without added sugar. A special pre-treatment of dipping of grapes in ethyl oleate (2% solution in 0.5% sodium hydroxide) at 80?deg; C for 30 s further reduced the drying time by factor 2 in both cases. The color of osmo-convective dried grapes were comparable to that of sulfur dioxide treated grapes. The texture of osmo-convective dried grapes was more pliable (softer) than convective dried samples. The major problem associated with die osmo-convective drying of grapes on a sugar bed was the stickiness, caused by sugar, on the fruit surface. This was reduced by partially substituting sugar with semolina (maintaining a 1:1 ratio) to create fluidized bed.
Keywords:Grapes  fluidized bed  kinetics  osmosis  quality
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