
FLUID-WALL AEROSOL FLOW REACTOR FOR HYDROGEN 459
carbon particles; that is,
2
h
∗
P
W
∗
C
U
∗
G
(T
∗
C
− T
∗
G
)
∼
=
87(T
∗
C
− T
∗
G
)
∼
=
1 ⇒ T
∗
C
− T
∗
G
∼
=
0.011 ⇒ T
∗
G
∼
=
0.99T
∗
C
(7.5-46)
Hence, the fluid-wall aerosol reactor can be modeled assuming that the gas is in
local thermal equilibrium with the carbon particles; that is, it is not necessary to
solve the thermal energy equation for the gas. However, note that this approximation
was based on the system parameters given in Table 7.5-1. For sufficiently large
particles and/or high reactor wall temperatures, the dimensionless group
2
will
become less than 1, implying that the gas temperature is much less than that
of the carbon. The conclusion that the gas and carbon particles are in thermal
equilibrium can also be obtained from the scaled thermal energy balance for the
gas phase since
8
1, which again implies that T
∗
G
∼
=
T
∗
C
. The fact that
2
1
and
8
1, both of which imply that T
∗
G
∼
=
T
∗
C
, confirms that we have chosen
our scales correctly for the process parameters given in Table 7.5-1. If one is
not aware that rapid thermal equilibrium is achieved between the gas and carbon
particles, serious problems can be encountered in solving the describing equations
numerically. For sufficiently large values of
2
there is a thermal boundary layer
at the entrance of the reactor wherein the gas and carbon particles come to thermal
equilibrium whose thickness is much less than the length of the reactor. Hence,
numerical integration employing a step size based on the reactor length will not
resolve the transport processes occurring in this boundary layer.
Let us now consider the temperature gradient in the reactor. This can be esti-
mated from equation (7.5-28). For the parameter values given in Table 7.5-1, we
obtain the following estimate:
T
Gzs
∼
=
T
Czs
=
εσa
C
M
C
ρ
H
S
c
(T
W
− T
0
)
4
(2W
0
M
+
ˆ
W
H
L)M
H
C
pCs
ρ
C
= 1163 K/m (7.5-47)
This estimate for T
Gzs
implies that the cloud of carbon particles and gas reach the
wall temperature before they exit from the downstream end of the reactor; that is,
z =
1200 K − 298 K
1163 K/m
= 0.78 m <L= 0.91 m (7.5-48)
Note that the temperature gradient increases markedly with increasing T
W
,which
implies that the gas and carbon particles will reach T
W
progressively farther
upstream as T
W
increases.
The dimensionless groups
1
,
5
,and
6
are of
◦
(1) and thus do not per-
mit us to conclude that the term they multiply, (1 −X
c
)
n
, is small; that is, we
cannot conclude from the magnitude of these groups that the conversion is nearly
complete. However, our scaling analysis allows us to estimate whether the reactor
is sufficiently long to achieve complete conversion of the methane. An estimate