Environmental Engineering Reference
In-Depth Information
The basic derivation in case of vaporization proceeds as follows. We start with the
observation that in a steady conversion, the mass flow rate,
r 2
m=4
_
π
ρ g v r , remains the
same in the gas surrounding the particle (continuity):
r 2
ρ g v r
=0
ð
Eq
:
9
:
14
Þ
r
Now, the energy equation can be written as a balance equation for convection and
diffusion, which in terms of temperature becomes
=0
ρ g D
T
r 2
r 2
ρ g v r T
ð
Eq
:
9
:
15
Þ
r
r
r
We can use continuity, r 2
ρ g v r = m
=
4
π
, to arrive at
=0
m
4
_
T
r
ρ g D
T
r 2
ð
Eq
:
9
:
16
Þ
π
r
r
and assume for the Lewis number, being Le =
is the ther-
mal conductivity and c p the specific heat capacity. Then Equation (9.16) becomes
λ
/(c p ρ g D ), Le = 1. Herein,
λ
=0
c p
λ
m
4
T
r
ρ g D
T
r 2
ð
Eq
:
9
:
17
Þ
π
r
r
Introducing Z =c p /(4
πλ
) and integrating give
r 2
T
r = Z
mT + C 1
_
ð
Eq
:
9
:
18
Þ
Integrating once again results in a solution for the temperature
=
C 1
Z _
m
r
Tr
ðÞ
m +C 2 exp
ð
Eq
:
9
:
19
Þ
Z
_
Boundary conditions can be formulated at the droplet surface and far away from the
droplet, T(r = r s )=T boil and T(r
!
)=T . Substituting these solutions, it is easy to
derive
T
T boil
r s
C 2 =
ð
Eq
:
9
:
20
Þ
Z m
1
exp
and C 1 =C 2
ð
T
Þ
Z
m, leading eventually to the temperature distribution
_
r s +T boil
Z m
r
Z m
ð
T
T boil
Þ
exp
T exp
r s
Tr
ðÞ
=
ð
Eq
:
9
:
21
Þ
Z m
1
exp
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