Abstract
The equation for the calculating of a moisture evaporation rate in the vacuum freeze-drying, wherein as a driving force instead of the generally accepted in the drying theory of ∆t temperature difference, ∆p pressure difference, ∆c concentration difference, a difference of water activity in the product and the relative air humidity (\(a_{\text{w}} - \varphi\)) is suggested. By using the proposed equation, the processes of vacuum freeze-drying of koumiss and shubat were analyzed, and it was found two drying periods: constant and falling. On the first drying period, a moisture evaporation rate of koumiss is j = 2.75 × 10−3 kg/(m2 h) and of shubat is j = 2.37 × 10−3 kg/(m2 h). On the second period, values decrease for koumiss from j = 2.65 × 10−3 kg/(m2 h) to j = 1.60 × 10−3 kg/(m2 h), and for shubat from j = 2.25 × 10−3 kg/(m2 h) to j = 1.62 × 10−3 kg/(m2 h). Specific humidity for koumiss is ueq = 0.61 kg/kg and for shubat is ueq = 0.58 kg/kg. The comparative analyze of the experimental data of the moisture evaporation rate versus the theoretical calculation shows that the approximation reliability is R2 = 0.99. Consequently, the proposed equation is useful for the analyzing a moisture evaporation rate during a vacuum freeze-drying of dairy products, including cultured milk foods.
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Abbreviations
- j :
-
Moisture evaporation rate from the product surface (kg/m2 h)
- µ :
-
Evaporation resistance coefficient
- \(a_{\text{w}}\) :
-
Water activity (%)
- φ :
-
Relative air humidity (%)
- u p :
-
Product specific humidity (%)
- \(L_{j,k} = \chi_{j,k}\) :
-
Kinetic coefficient
- \(L_{j,k} = D_{j,k}\) :
-
Kinetic coefficient
- ∇ C:
-
Concentration gradient
- ∇ t :
-
Temperature gradient
- σp :
-
Moisture evaporation rate from the product, kg/(m2 s)
- \({\text{d}}_{\text{p}}^{\prime \prime }\), \({\text{d}}_{a}^{\prime \prime }\) :
-
Moisture content of saturated air at the product surface
- C p :
-
Isobaric specific heat of air [J/(kg K)]
- \(\alpha\) :
-
Coefficient of heat transfer from the product surface [W/(m2 K)]
- B :
-
Barometric pressure (Pa)
- Wi :
-
Initial moisture for koumiss (Wi = 91.0), and for shubat (Wi = 88.0) (%)
- Wp :
-
Product humidity at the measuring time (%)
- Wcr :
-
Moisture at the critical point (%)
- A:
-
Constant coefficient, A = 0.622·α·B−1, W/(m2 K Pa)
- i:
-
Initial value
- T:
-
Temperature (C)
- P″a:
-
Partial pressure of water vapor in the air (Pa)
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Shingisov, A.U., Alibekov, R.S. Analysis of the moisture evaporation process during vacuum freeze-drying of koumiss and shubat. Heat Mass Transfer 53, 1571–1578 (2017). https://doi.org/10.1007/s00231-016-1920-4
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DOI: https://doi.org/10.1007/s00231-016-1920-4