
348 APPLICATIONS IN MASS TRANSFER
its local concentration in the latter is equal to εc
A
,inwhichε is the porosity
and c
A
is the local concentration of oxygen in the pores. Owing to the microp-
orous structure, the effective oxygen diffusivity in the rust, which is denoted by
D
AC
, will be less than that in the water, which is denoted by D
AB
. The densi-
ties of the water, water-saturated rust, and pure iron are denoted by ρ
B
,ρ
C
,and
ρ
D
, respectively, in which B, C,andD denote the water, rust, and iron, respec-
tively. The corresponding molecular weights are denoted by M
B
,M
C
,andM
D
,
respectively. Note that this problem involves two moving boundaries: the interface
between the rust and the water and that between the iron and the rust, as shown
in Figure 5.P.17-1. One might anticipate that initially, oxygen diffusion through
the water controls the rate of rusting, whereas at longer times, oxygen diffusion
through the rust becomes controlling. We use scaling analysis to explore how the
describing equations for this mass-transfer process can be simplified. In scaling this
problem, use the following dimensionless variables involving unspecified scale and
reference factors:
c
∗
AW
≡
c
A
− c
Wr
c
Ws
; c
∗
Ar
≡
c
A
− c
Rr
c
Rs
; z
∗
W
≡
z − z
Wr
z
Ws
;
z
∗
R
≡
z − z
Rr
z
Rs
; t
∗
≡
t
t
s
; (5.P.17-3)
L
∗
R
≡
L − L
R
L
Rs
; L
∗
I
≡
L
L
Is
;
dL
dt
∗
R
≡
1
˙
L
Rs
dL
dt
R
;
dL
dt
∗
I
≡
1
˙
L
Is
dL
dt
I
where the subscripts W, R,andI refer to the water, rust, and iron layers, respec-
tively.
(a) Explain why it is necessary to define separate reference and scale factors
for the concentrations and spatial coordinates in the water and rust layers.
(b) Explain why it is necessary to define separate scale factors for the thick-
nesses of the rust and iron layers as well as the velocities of each layer.
(c) Write the appropriately simplified species-balance equations and their initial
and boundary conditions for both the water and the rust layer; use molar
concentrations and assume dilute solutions so that the bulk-flow contribution
to the mass-transfer flux can be ignored.
(d) Carry out an integral mass balance on the iron and rust layers to obtain the
auxiliary equations required to determine the location of the two moving
boundaries. Note that the growth rate of the rust layer must satisfy the
molar exchange dictated by reaction (5.P.17-1).
(e) Use scaling analysis to estimate the thickness of the region of influence in
the water layer.
(f) Determine the criteria for quasi-steady-state to apply.