Chapter 3 Diffusion in concentrated solutions page 3-5
8. Mass balance assumptions
(a) Steady flow and unsteady mass transfer in a tube.
(c) The terms are
accumulation = (axial flow in – out)
+ (radial diffusion in – out)
+ (axial diffusion in – out).
Radial, diffusion-induced flow is sensibly neglected.
9. Porous solid desiccant
2
0
0.5
1
3
02468
t
1/2
When using a semi-infinite slab model, from Eq.
The absorbed amount
M = 0
t N1Adt = 2 Dt A/V1
As observed on the right figure, this model does
not fit the experimental data. Instead, as the
problem states, we assume that the slab contains
cylindrical pores in which water can diffuse fast.
The flux out of these pores is given by Eq. 5.80
in Crank’s book (p. 87):
D
where a is the radius of the pore. Integration gives
t j1dt = M0 + A
4Dt
As the figure shows, these data fit very well to this equation. Thus,
c = 0.1759 g/min = 0.00126 mol/s
The surface area of the slab is
At 45 °C, p(sat) = 0.0946 atm,