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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