Environmental Engineering Reference
In-Depth Information
=
Rate of accumulation
X
m
i
c
p
,
i
dT
dt
Rate of supply = 0
ð −
rate of release = 0
ðÞ
+
Þ
Q
Rate of production V
ð
−
Δ
r
H
Þ −
ð
R
A
X
A
,T
ð Þ
Þ
Þ
+ heating or cooling
ð
ð
Eq
:
6
:
14
Þ
The term
Q
represents any addition or removal of heat from the reactor. The energy
balance states that the variation of temperature in the reactor (dT/dt) depends on four
key factors, namely, the rate of heat generation V(
R
A
(
X
A
, T)), the heat added
to or removed from the system
Q
, the mass of the species m
i
, and the specific heat
capacity of the species involved c
p
,i
, which in this case is considered constant.
A strongly exothermic reaction such as combustion (
−
Δ
r
H
)(
−
Δ
r
H
has a large negative value)
will increase (dT/dt) unless the removal of heat
Q
counteracts the production of heat.
The term
Q
can be manipulated to get the desired (dT/dt) in the reactor by heating the
reactor or cooling it.
The solution of the energy balance leads to
X
m
i
c
p
,
i
dT
+
Q
dt
=V
ð
−
Δ
r
H
Þ −
ð
R
A
X
A
,T
ð Þ
Þ
ð
Eq
:
6
:
15
Þ
For adiabatic systems,
Q
= 0. If the reactor is heated/cooled by interchanging
heat with an external fluid, e.g., through a heat exchange coil,
Q
will have the form
Q
=
hA
T
f
−
.T
f
is the temperature of the heating/cooling fluid, T is the temperature
of the reactor,
h
is the heat transfer coefficient, and
A
is the heat exchange area.
Substituting Equation (6.12) in Equation (6.15), we obtain
ð Þ
T
X
m
i
c
p
,
i
dT
n
A0
d
X
A
dt
=
Q
dt
−−
Δ
r
H
ð
Þ
if = 0
!
adiabatic
ð
Eq
:
6
:
16
Þ
Thus,
=
ð
t
X
m
i
c
p
,
i
T
Q
dt
Tð Þ−−
Δ
r
H
−
ð
Þ
n
A0
X
A
−
ð
X
A
0
Þ
0
=
Q
t
ð
Eq
:
6
:
17
Þ
Q
= constant
ð
if
Þ
if = 0
!
adiabatic
Although in some cases it is possible to obtain an analytical solution, most of the cases
require numerical methods to solve the combined mass and energy balances.
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