Chapter 2 Diffusion in dilute solutions page 2-1
Chapter 2 Diffusion in dilute solutions
1. Water evaporation
To find the rate of evaporation, we need to find the flux of water across the air film:
11 c
DH
jΔ= l
Since the film is made up of air, H = 1. We are given D and ℓ, so we need to find Δc1. We first
calculate the difference in the partial pressure of water across the film. From a steam table we
find that at 20 °C, psat = 2.3388 kPa. Since the air immediately above the water is saturated we
1
Assuming an ideal gas, we can find the concentration difference:
()
3
7
3
1
1108.448.0
2933145.8
4.1169
cm
mol
m
mol
K
molK
J
Pa
RT
p
⎟
⎠
⎞
⎜
⎝
⎛
⋅
Δ
We can now calculate the flux:
scm
mol
cm
mol
cm
s
cm
j2
7
3
7
2
1100.8108.4
15.0
25.0 −− ⋅=
⎟
⎠
⎞
⎜
⎝
⎛⋅=
To find the height change, we divide by the molar density of water:
cm
s
cm
g
mol
cm
g
scm
mol
015.18
1
1
100.8 5
3
2
7
⋅
⋅−
−
2. Diffusion across a monolayer
Recalling that the resistance is the inverse of the permeance, we have:
s
cm
P
cm
s
P5.02
1=⇒=
We know that the permeance is given by:
()
cm
cm
s
cm
P
DH
2
6
7
105.25.0
−
−
⋅
⎟
⎠
⎞
⎜
⎝
⎛
3. Diffusion coefficient of NO2 in water
We treat the water as a semiinfinite slab. From Eq. (2.3-18) we know that the flux at the surface
is given by: