Steady State Mass Transfer – Other Geometries
2026-01-19
(Continue from Lecture 06) After today’s lecture, you will be able to:
Steady state mass balance
Many industrial applications involde 1D transport with variable area \(A(z)\), with mass balance:
\[\begin{align} [\mathrm{In}] - [\mathrm{Out}] &= 0 \\ N_{A1} A_1 - N_{A2} A_2 &= 0 \end{align}\]Define the total molar flow rate of A:
\[ \overline{N}_A = N_A \, A(z) \]
At steady state: - \(\overline{N}_A\) is constant - \(N_A\) varies with position if \(A(z)\) (or \(A(r)\)) varies
This framework can be used to solve diffusion through:
Key ideas
Typical physical situations
Conditions
Governing equation (stagnant B): use the ODE form, not the full 1D Cartesian solution:
\[\begin{align} N_A &= -\frac{D_{AB}}{RT}\frac{d p_A}{dr} + \frac{p_A}{p_T} N_A \\ N_A\!\left(1 - \frac{p_A}{p_T}\right) &= -\frac{D_{AB}}{RT}\frac{d p_A}{dr} \end{align}\]For spherical symmetry, \(N_A(r)\) varies with \(r\) and cannot appear alone in the balance equation L.H.S
Use the constant molar flow rate: \[ \overline{N}_A = N_A(r)\,4\pi r^2 = \text{constant} \]
\[\begin{align} \frac{\overline{N}_A}{4\pi r^2}\,dr &= -\frac{D_{AB}}{RT}\frac{1}{1-p_A/p_T}\,dp_A \end{align}\]This looks very similar to the 1D stagnant B solution in cartesian coordinates. We can simplify it in several occations.
Special case: \(r_2 \gg r_1\) (often \(r_2 \to \infty\))
Typical examples: - Evaporating liquid droplet - Sublimation of a naphthalene (solid) sphere
From the general spherical stagnant-B result, use the log-mean pressure form:
\[\begin{align} \boxed{ N_{A1} = \frac{D_{AB} p_T}{RT\,p_{Bm}} \left(p_{A1} - p_{A2}\right) } \end{align}\]Where \(N_{A1} = N_A(r=r_1)\). For liquid, another form is often used (considering \(p_{Bm}/p_T \approx 1\) and use \(p = cRT\))
\[\begin{align} \boxed{ N_{A1} = \frac{D_{AB}}{r_1}\left(c_{A1} - c_{A2}\right) } \end{align}\]Special case: thin membrane / shell
\(\Delta r = r_2 - r_1 \ll r_1\)
Approximation: \[ \frac{1}{r_1} - \frac{1}{r_2} \;\approx\; \frac{r_2 - r_1}{r_1^2} \;=\; \frac{\Delta r}{r_1^2} \]
Final result:
\[\begin{align} \boxed{ N_{A1} = \frac{D_{AB}}{RT}\frac{p_T}{p_{Bm}} \frac{(p_{A1}-p_{A2})}{\Delta r} } \end{align}\]This acts like a 1D stagnant-B film with thickness \(\Delta r\)! (See lecture 3 wooclap question.)
Conditions:
Assume linear radius profile: \[ r(z) = r_1 + \frac{(r_2-r_1)}{(z_2-z_1)}(z-z_1) \]
Use the ODE form with \(\dot N_A = N_A(z)\,A(z)\) and \(A(z)=\pi r(z)^2\):
\[\begin{align} \frac{\dot N_A}{\pi}\int_{z_1}^{z_2}\frac{dz}{\left[r(z)\right]^2} &= -\frac{D_{AB}}{RT}\int_{p_{A1}}^{p_{A2}} \frac{dp_A}{1-p_A/p_T} \end{align}\]Can you solve for \(N_{A1}\)?
Adapted from Geankoplis 6.2-3
Water vapor diffuses through a stagnant gas in a narrow vertical tube, dry air is constantly blown at the top of tube.
At time \(t\), the liquid level is a distance \(z\) from the tube top (i.e., the diffusion path length is \(z\)).
As diffusion proceeds, the liquid level drops slowly, so \(z\) increases with time. The liquid has density \(\rho_A\), and molecular weight \(M_A\)
Tip
Answer \[ t_F = \frac{\rho_A (z_F^2 - z_0^2) RT p_{Bm}}{2 D_{AB} M_A p_{T}} \frac{1}{(p_{A1} - p_{A2})} \]
Adapted from Griskey 10-2
Sample setup as example 4, a vertical tube of diameter \(D=0.01128\) m contains a liquid volatile species \(A\) (chloropicrin, \(CCl_3NO_2\)) evaporating into stagnant air (\(B\)) at 1 atm. The gas-phase diffusion of \(A\) occurs through the air column above the liquid surface.
At \(t=0\), the distance from the tube top to the liquid surface is \(z_0 = 0.0388\) m, after \(t=1\) day, the distance is \(z_1 = 0.0412\) m.
Tip
Pseudo steady state solution and assuming \(N_A=\text{const}\) solution differ very little. Why?
Answer:
Adapted from Geankoplis Ex 6.2-4
A sphere of naphthalene having a radius of 2.0 mm is suspended in a large volume of still air at 318 K and \(1.01325 \times{}10^5\) Pa (1 atm). The surface temperature of the naphthalene can be assumed to be at 318 K and its vapor pressure at 318 K is 0.555 mm Hg. The \(D_AB\) of naphthalene in air at 318 K is \(6.92\times{}10^{−6}\ \text{m}^2/\text{s}\).
Tip
Similar setup as example 5. \(N_A\) is time-dependent
Answer:
Compare the solutions with Example 4. We can also measure the diffusivity of volatile organic molecules using the sphere evaporation methos!