The physical data taking part in heat transfer vary with temperature, and some to a large extent. Therefore, the estimation of temperature distribution in packed bed extending over wide temperature cannot be obtained accurately, unless the variation of physical data is known. We took these into consideration, and discussed possible mathematical ways which are related to heat transfer of such a nonlinear type.
For those assumptions that axial diffusion and temperature difference between fluid and particle are neglected, we made the following two models.
i)
Q=0, and λ
er/
K' is a linear function of the cross sectional average temperature.
ii)
Q, λ
er/
K', and λ
er/
U are arbitrary functions of local temperature.
Then, model i) can be expressed by these fundamental equations (9)-(11), (Eq.(13)-15) are of their dimensionless form). This problem is not difficult to solve analytically if some approximation could be permitted. We obtained these approximate analytical solutions (30)-(32). Improvement in these equations is projected by the term
F (
s)(Eq.(28)) and the value of
F (
s) can be drawn on a graph (Fig. 1) with axial distance Aζ
21s and alienate parameter (
B/A)θ
m0. Furthermore, in order to compare the projected
F (
s) with that of linear model, three curves are shown in Fig. 2. The curve (I) is for the case of (
B/A)θ
m0=5, (II) is for (
B/A)θ
m0=-0.833 and (III) for (
B/A)θ
m0=0 taking
A' the arithmetic mean value of
k (
s).
The equation (34)-(36) are the fundamental equations of model ii). These equations can be developed to (37)-(43). The solution of these equations can not be obtained by any analytical method. The method only remained for us would be numerical calculation. Then, equation (34) is transformed to difference equation (44). The situation changes depending upon whether Δ
z/Δ
r2k (
t) is less than 1/2 or not.
Case 1)Δ
z/Δ
r2k (
t)≤1/2. If we denote the incremental value of
t as Eq.(45), the equation (44) may be solved as (46). The boundary condition defined by Eq.(36) also gives (47)-(49).
Case 2)Δ
z/Δ
r2k (
t)<1/2. We recall here to Neumann's method. If we denote Δ
2rt as the equation (53) and prescribe the boundary condition in the same way from case 1), a set of simultaneous linear algebral equation (55) for each step in z is obtained.
Applying these solutions, we computed a temperature distribution for an example, and showed their results in Fig.3.
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