Introduction & Context
The Critical Freezing Rate Determination is a fundamental calculation in food process engineering and cryogenics. It is used to predict the time required for a product, modeled as a one‑dimensional infinite slab, to transition from its initial freezing point to a target core temperature. This process is critical for maintaining product quality, as rapid freezing minimizes ice crystal size, thereby preserving cellular structure and texture in biological materials like fish fillets or meat products, and underscores the importance of selecting proper packaging for frozen foods to protect quality during storage and distribution.
This calculation is typically employed during the design phase of industrial blast freezers and contact freezing systems to ensure that the cooling capacity is sufficient to meet safety and quality standards within a specified time frame.
Methodology & Formulas
The determination of the total freezing time is divided into two distinct physical phases: the latent heat removal phase (front arrival) and the sensible cooling phase of the frozen core.
1. Biot Number
The Biot number determines the ratio of internal conductive resistance to external convective resistance. It dictates whether the system can be treated as a lumped mass or if internal temperature gradients must be considered.
\[ Bi = \frac{h \cdot L}{k_{\text{frozen}}} \]2. Freezing Front Arrival Time (Plank's Equation)
Based on Plank's equation for an infinite slab, this phase accounts for the time required for the freezing front to propagate from the surface to the thermal center, primarily driven by the removal of latent heat of fusion.
\[ t_{\text{front}} = \frac{\rho \cdot h_{sf}}{T_{f} - T_{\infty}} \cdot \left( \frac{L}{h} + \frac{L^{2}}{2 \cdot k_{\text{frozen}}} \right) \]3. Sensible Cooling Time (First-Term Series Solution)
Once the freezing front reaches the center, the core undergoes sensible cooling from the freezing point to the target temperature. This is calculated using the first-term series solution for a slab with convective boundary conditions, requiring the determination of the first eigenvalue \(\zeta_{1}\) and the coefficient \(C_{1}\).
\[ t_{\text{sens}} = \frac{L^{2}}{\alpha_{\text{frozen}} \cdot \zeta_{1}^{2}} \cdot \ln\left( \frac{C_{1} \cdot (T_{f} - T_{\infty})}{T_{c} - T_{\infty}} \right) \]Where the thermal diffusivity of the frozen product is defined as:
\[ \alpha_{\text{frozen}} = \frac{k_{\text{frozen}}}{\rho \cdot c_{p,\text{frozen}}} \]The eigenvalue \(\zeta_{1}\) is the first positive root of the transcendental equation for a plane wall:
\[ \zeta_{1} \cdot \tan(\zeta_{1}) = Bi \]The first-term series coefficient \(C_{1}\) is calculated as:
\[ C_{1} = \frac{2 \cdot \sin(\zeta_{1})}{\zeta_{1} + \sin(\zeta_{1}) \cdot \cos(\zeta_{1})} \]4. Total Zone Passage Time and Cooling Rate
The total time to pass through the critical freezing zone is the sum of the front arrival time and the sensible cooling time.
\[ t_{\text{zone}} = t_{\text{front}} + t_{\text{sens}} \]The average cooling rate across the critical temperature zone (in K/min) is:
\[ \text{Cooling Rate} = \frac{T_{f} - T_{c}}{t_{\text{zone}} \, / \, 60} \]Regime Validity and Constraints
| Parameter | Condition | Implication |
|---|---|---|
| Biot Number (\(Bi\)) | \(Bi \lt 0.1\) | Internal gradients negligible; lumped capacitance model is sufficient. |
| Biot Number (\(Bi\)) | \(0.1 \le Bi \le 10\) | Distributed-parameter model required. Plank's equation and the convective series solution are valid. |
| Biot Number (\(Bi\)) | \(Bi \gt 10\) | External resistance negligible; constant surface-temperature (\(T \approx T_\infty\)) assumption applies. |
| Fourier Number (\(Fo\)) | \(Fo \lt 0.2\) | First-term series approximation is insufficient; higher-order terms or numerical methods required. |
| Fourier Number (\(Fo\)) | \(Fo \ge 0.2\) | First-term series approximation is valid (error < 2%). |