Fundamentals of mass diffusion
1 Errata
Section titled “1 Errata”-
Slide 11 has an incorrect species subscript in the mass-fraction denominator. Use
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Slide 13 retains species subscripts on the summed mixture fluxes. Use the total fluxes
The molar-flux description should say molar flow rate per unit area.
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Slide 14 mislabels the second velocity heading. Use “Molar-average velocity” with
2 Reading list
Section titled “2 Reading list”- Bird et al. (2006), chapters 17 and 18.
- Geankoplis (2003), chapter 6.
- Welty et al. (2001), chapter 24.
Use consistent kmol units with .
3 Choose a steady-diffusion model
Section titled “3 Choose a steady-diffusion model”| Given conditions | Model and checks |
|---|---|
| Equal and opposite molar fluxes | Set total molar flux to zero and use Eq. 8. |
| Carrier B has zero net flux | Retain bulk molar motion and use the stagnant-carrier logarithmic relation, Eq. 9. |
| Radial transfer through a cylinder or sphere | Write an area-weighted shell balance; conserve molar rate rather than radial flux. |
| A liquid boundary moves slowly | Use a pseudo-steady gas profile plus the interface inventory balance, Eq. 11. |
| Concentration changes through time inside a body | Move to the transient-diffusion topic; a steady film model alone is insufficient. |
4 Fick’s law of diffusion
Section titled “4 Fick’s law of diffusion”When two gases with different compositions meet, random molecular motion mixes them even if there is no imposed flow. Across a plane in the gas, molecules of A arrive from both sides. More arrive from the side with the greater concentration of A, so their random motion produces a net transfer towards the lower concentration.
Fick’s law relates that net transfer to the concentration gradient. For a binary mixture at constant total molar concentration, the molar diffusive flux relative to the mixture’s molar-average velocity is
is in , in , in m and in . The gradient has units , so the dimensions close. The minus sign predicts transport down the gradient. The specified reference frame matters. A moving mixture can also transport A past the tube wall, so the flux measured by a fixed observer may differ from .
At constant total molar concentration, decreases as increases and . What is the direction of the molar diffusive flux ?
Explanation
Fick’s law gives
The concentration gradient is negative, so the diffusive flux is positive. A moves toward increasing position, from higher to lower concentration. Bulk motion can make the total flux different from this diffusive flux.
4.1 Examples: estimating diffusion times
Section titled “4.1 Examples: estimating diffusion times”Diffusion smooths a concentration difference over a distance on the time scale
The estimate follows by comparing the accumulation term with the diffusion term in the transient species balance. It estimates how quickly a profile changes, rather than the exact time to reach a specified concentration.
For , the estimate gives
The values of are illustrative. Diffusivity depends on the species pair, phase and temperature. Over the same distance, molecular diffusion can mix a gas in a fraction of a second while taking years in a solid. Doubling the distance multiplies the estimated time by four.
For modest dilute-gas extrapolations, kinetic theory gives
Use absolute temperatures and matching pressure units. Doubling temperature at fixed pressure predicts a factor 2.83 with this estimate, compared with 3.36 using a fit. Measured data take precedence.
For hydrogen in nickel, at and at . Solid-state diffusion is often represented by the Arrhenius relation,
Taking logarithms at the two temperatures eliminates the unknown prefactor . The activation energy is therefore
Thus the two supplied values imply . The gas constant here is on a molar basis, .
For a porous medium using
and give .
A species has constant diffusivity . What is the diffusion time scale across mm?
Explanation
First convert the diffusion distance:
Then estimate the diffusion time:
5 Units of concentration terms
Section titled “5 Units of concentration terms”Let be species mass concentration in , molar concentration in , molecular weight in kg kmol⁻¹, and the dimensionless mass fraction. The source also writes for the same fraction. Use for gas mole fraction and for liquid mole fraction; a general mixture mole fraction below is denoted . The source shell balance uses even for gas, which denotes the same quantity as our .
The total mass and molar concentrations are sums over the species,
The mass fraction and mole fraction are the corresponding species-to-total ratios,
Both sets of fractions sum to one,
For an ideal gas , and . Here is partial pressure and total pressure in Pa; . For a liquid, , where is the mixture molecular weight, not the solute’s molecular weight. Conversion between mass and mole fractions follows
In a binary mixture , so the gradients are opposite. At constant , this identity and require the same mutual diffusivity for the pair. They do not imply that laboratory-frame total molar flux is zero.
A binary mixture contains equal moles of A and B, but A has the greater molar mass. Which statement is true?
Explanation
Mole fraction counts moles, while mass fraction weights those moles by molar mass. Equal molar amounts therefore give equal mole fractions and unequal mass fractions when molar masses differ.
6 Component velocity in a mixture
Section titled “6 Component velocity in a mixture”A species velocity in m s⁻¹ is a local average of many random molecular velocities, leaving a small drift. It is not a molecule’s thermal speed. A fixed observer measures mass flux in or molar flux in . Their sums and describe the mixture.
The two mixture averages weight different quantities:
is the mass-average velocity used in overall mass continuity; is the molar-average velocity natural for molar diffusion. In an equal-mole hydrogen/nitrogen mixture with and molecular weights 2 and 28, but
These averages coincide when molecular weights are equal.
A fixed observer sees , a mass-average observer sees , and a molar-average observer sees . A diffusion velocity measures the species drift relative to the chosen mixture average. It can be positive, negative or zero. Weighted sums of diffusion velocities vanish by construction.
7 Bulk flux and diffusion flux
Section titled “7 Bulk flux and diffusion flux”By Eq. 5, . Expanding gives
so
Figure 1 shows how transport by bulk motion and diffusion add to give the total molar flux in Eq. 6. For stagnant B, the bulk contribution is the fraction of . For arbitrary , use the full sum to determine the bulk contribution. At dilute A the stagnant-carrier correction is small because A makes up only a small fraction of the moving mixture. At higher concentrations, it must be included.
In a binary mixture, the molar-frame diffusive fluxes satisfy . What follows about the total molar flux past a fixed observer?
Explanation
The diffusive fluxes sum to zero in the molar-average frame. Past a fixed observer, bulk motion also transports material:
The total molar flux can therefore be nonzero. It is zero only if the molar-average velocity is zero, as in equimolar counter-diffusion.
8 Diffusion flux
Section titled “8 Diffusion flux”Substituting Eq. 1 into Eq. 6 gives
The product derivative
explains the constant- restriction. In an isothermal isobaric ideal gas it is exact. A liquid may need a composition-dependent model or a justified average concentration. Positive flux means motion in positive ; a negative result reports the direction rather than an arithmetic failure.
9 Diffusion flux: two limiting cases
Section titled “9 Diffusion flux: two limiting cases”Equimolar counter-diffusion imposes . Burning solid carbon to only carbon dioxide consumes one oxygen molecule for one carbon dioxide molecule produced, so this is a useful gas-film model. Formation of CO changes the ratio and invalidates the equimolar assumption. Binary distillation with equal molar latent heats is another approximate example.
A crossing stagnant B imposes . Water absorbed into concentrated acid crosses the interface while insoluble carrier air does not. Air can still diffuse towards the interface: bulk motion cancels its diffusion exactly. This is zero net flux, not zero microscopic motion. Other stoichiometric ratios or imposed flows must be inserted into Eq. 7 explicitly.
10 Equimolar counter-diffusion of gases A and B
Section titled “10 Equimolar counter-diffusion of gases A and B”Take steady, one-dimensional, nonreacting transfer across with constant , and . Conservation makes constant. Since ,
Partial pressures and concentrations are linear, with . The pressure-based resistance is , with units , while concentration-based resistance has units s m⁻¹. Use the same driving-force basis when adding resistances in series.
11 A diffusing through stagnant, non-diffusing B
Section titled “11 A diffusing through stagnant, non-diffusing B”Now set in Eq. 7. Rearranging and separating gives
Equivalently
When , the logarithm is positive. The local multiplier is 2 at and 10 at 0.9. At low concentration the logarithm approaches and Eq. 8 returns.
Define the log-mean stagnant-species partial pressure and mole fraction:
If the endpoints coincide, take the common value as the log mean. The exact enhancement is , not an arbitrarily chosen local fraction. The logarithm follows from integrating and the profile is curved. Its gradient magnitude increases towards the low-A end because
The smaller fraction of A at that end means that a steeper gradient is needed to maintain the same total flux.
As A becomes dilute, approaches one; when B’s log-mean fraction is 0.5, . This correction needs the stagnant-B model. A change in reaction stoichiometry or imposed bulk flow changes the multiplier.
A diffuses through stagnant B with . What does stagnant mean here?
Explanation
Stagnant B means that no net amount of B crosses a fixed surface. B can still diffuse in one direction while bulk motion carries it in the opposite direction. These contributions cancel. It does not mean that B molecules stop moving or that the mixture has zero bulk velocity.
11.1 Pseudo-steady-state analysis with a moving boundary
Section titled “11.1 Pseudo-steady-state analysis with a moving boundary”Let be the distance from a falling pure-liquid surface to a fixed swept tube mouth. The surface equilibrium composition and the mouth composition remain constant. The gas adjusts over while the liquid retreats much more slowly, so approximate the gas profile as steady at each instantaneous length. Liquid molar density is , with a mass density, not a molar density.
Since
this also reproduces the source’s log-mean form. Only changes during integration. Plotting against time is the Stefan-tube method of estimating diffusivity. Its slope is . Maintaining temperature, a dry mouth and negligible convection is necessary.
12 Classroom example 1: water evaporation
Section titled “12 Classroom example 1: water evaporation”Water evaporation
Section titled “Water evaporation”Water in the bottom of a narrow metal tube is held at a constant temperature of 293 K. The total pressure of air (assumed dry) is and the temperature is 293 K. Water evaporates and diffuses through the air in the tube, and the diffusion path is 0.1524 m. Calculate the rate of evaporation at steady state in . The diffusivity of water vapour at 293 K and 1 atm pressure is . Assume that the system is isothermal. The vapour pressure of water at 1 atm and 293 K is 17.535 mmHg.
Additional note: Moving boundaries or pseudo-steady state diffusion. How long would it take for the water level to decrease by 0.1 m?
Solution
The evaporation path is the gas space between the water surface and the tube mouth, as shown in Figure 2. Water vapour moves upwards. Air has zero net flux across the liquid interface.
Data
| Quantity | Value |
|---|---|
| Initial gas diffusion length | |
| Temperature | |
| Pressure | |
| Diffusivity | |
| Surface vapour pressure | |
| Liquid density for the moving-boundary calculation | |
| Water molar mass | |
| Final gas diffusion length |
The source unit kgmol is equivalent to kmol. Liquid density and molar mass are supplementary inputs needed to convert liquid-depth loss to an amount evaporated.
Assumptions
- Unidirectional diffusion through the gas space.
- Steady gas profile for the initial flux calculation.
- Pseudo-steady gas profile as the liquid surface recedes.
- Ideal gas behaviour.
- Constant temperature, pressure and diffusivity.
- Vapour-liquid equilibrium at the water surface.
- Zero net air flux through the liquid surface.
- Negligible natural convection.
Calculations
At the liquid surface, equilibrium fixes the vapour partial pressure. At the mouth, the dry air gives . Converting the surface vapour pressure to Pa gives
The surface mole fraction and total gas concentration are
Because air has zero net flux, the appropriate governing relation is the stagnant-carrier result, Eq. 9,
Substituting the boundary fractions and the initial gas length gives
Multiplying by molar mass converts the molar flux to mass flux,
The initial rate is about per day. The stagnant-carrier flux is only 1.17 percent above the equimolar estimate because the water vapour is dilute.
For the falling liquid level, the gas length increases and the evaporation flux decreases. Define the constant logarithmic driving force,
The liquid molar density is
A decrease in liquid depth removes kmol per unit tube area. Equating that loss to the instantaneous evaporation flux gives
Separating variables and integrating between the initial and final levels gives the moving-boundary relation, Eq. 11,
Substitute the consistent kmol-based concentrations,
As a check, removing of water requires . Even if the initial flux stayed constant, evaporation would take
The falling level lengthens the diffusion path, so the calculated time must be greater than that lower bound.
The gas diffusion time is , much shorter than the liquid retreat time. This supports the pseudo-steady approximation. Maintaining the stipulated isothermal, convection-free conditions for 536 days would be difficult in an experiment.
Answer
The initial evaporation flux is , directed towards the tube mouth. The corresponding mass flux is .
Under the pseudo-steady moving-boundary model, the water level takes , or about 536 days, to fall by .
13 Classroom example 2: butanol in water
Section titled “13 Classroom example 2: butanol in water”Butanol in water
Section titled “Butanol in water”Calculate the rate of diffusion of butanol at under unidirectional steady state conditions through a 0.1 cm thick film of water when the concentrations of butanol at the opposite sides of the film are, 10% and 4% butanol by weight, respectively.
(butanol in water solution)=. The densities of 10% and 4% butanol solutions at may be taken as 0.971 and 0.992 g/cc, respectively. Molecular weight of Butanol is 74, and that of water is 18.
Solution
Data
| Quantity | Value |
|---|---|
| Film thickness | |
| Diffusivity | |
| Butanol mass fraction at side 1 | |
| Density at side 1 | |
| Butanol mass fraction at side 2 | |
| Density at side 2 | |
| Butanol molar mass | |
| Water molar mass |
Assumptions
- Steady state.
- Unidirectional diffusion across the film.
- Isothermal conditions at .
- No chemical reaction.
- Zero net water flux.
- Constant diffusivity.
- Total molar concentration approximated by its arithmetic mean across the film.
Calculations
Let A be butanol and B be water, with positive flux from the 10 percent side to the 4 percent side. The stagnant-water model uses mole fractions, so first convert the supplied mass fractions. On a basis, side 1 contains mol butanol and mol water. Hence
For side 2, the same conversion gives
The total molar concentration equals the total moles divided by the solution volume. Since a sample occupies ,
Their arithmetic mean is
The total molar concentration changes by about 7 percent across the film. Treating it as uniform is an approximation for this liquid mixture. Constant temperature and pressure alone do not make a liquid’s molar concentration constant.
With zero net water flux, the governing total-flux relation is
Integrating over the film gives the liquid version of Eq. 9,
Substituting in centimetre and mol units gives
The mass flux follows by multiplying by the molar mass of butanol,
As a check, neglecting the stagnant-water correction gives
The full result is 1.85 percent larger, consistent with dilute butanol.
The flux is about per day. Comparing it with the water-evaporation example requires the concentration difference and film thickness as well as the diffusivity.
Answer
Butanol diffuses from the 10 percent side to the 4 percent side at , equivalent to a mass flux of .
14 Steady-state mass transport: shell balance approach
Section titled “14 Steady-state mass transport: shell balance approach”14.1 Species balance and homogeneous reaction
Section titled “14.1 Species balance and homogeneous reaction”At steady state, species inflow minus outflow plus generation is zero. Total already includes convection and diffusion. For a plane shell of area and thickness ,
is net production in , negative for consumption. A homogeneous th-order rate may be written , with units . Multiplying by volume produces kmol s⁻¹, while multiplying by face area produces the same units. A heterogeneous reaction acts at a boundary, so it sets a surface-flux condition instead of a volumetric source. A porous catalyst can distribute internal reacting area throughout its modelled volume, requiring an effective volumetric rate and diffusivity.
14.2 Setting interface conditions
Section titled “14.2 Setting interface conditions”Use the equilibrium relation appropriate to the example, such as Raoult’s law or Henry’s law , with in Pa for this convention. An impermeable face has ; a reacting face has a flux condition from its stoichiometry.
15 Case study 1: diffusion through stagnant gas film
Section titled “15 Case study 1: diffusion through stagnant gas film”15.1 Balance and constitutive law
Section titled “15.1 Balance and constitutive law”Consider the same straight tube at an instant, with interface and mouth . B cannot cross the liquid surface; steadiness without reaction then requires throughout. A’s balance is Eq. 16 with , so . Every mole leaving the liquid reaches the mouth. Substitute Eq. 7:
The isothermal isobaric gas has constant , and constant diffusivity is assumed. Remove these constants before integrating. If properties vary strongly they must stay inside the derivative.
15.2 Two integrations and boundary conditions
Section titled “15.2 Two integrations and boundary conditions”Integrating Eq. 17 once and then again gives
has units and is dimensionless. At and , impose and . Subtraction yields
Write the profile using a dimensionless distance measured from the liquid surface:
The endpoints give the specified values, and differentiating the profile reproduces Eq. 9 at every position. This is the benefit of shell balance: the profile is now known, rather than only a resistance formula. Dilute A makes it approximately linear.
16 Case study 2: steady-state diffusion from a suspended droplet
Section titled “16 Case study 2: steady-state diffusion from a suspended droplet”Take a spherical liquid droplet of radius surrounded by a gas film ending at radius . Radial coordinate points outward. Assume quasi-steady spherical symmetry, constant and , no reaction or external flow, interface gas fraction and outer fraction , and insoluble B. At a pure-liquid interface Raoult’s law sets the surface vapour fraction at the droplet temperature. A shrinking droplet is only instantaneously steady; neglect thermal cooling or include it in a coupled model.
A shell has different inner and outer areas. Conservation gives
Thus the flux falls as while total molar rate stays fixed. Substituting and integrating gives
Here has units m, unlike the plane integration constant. Subtract the surface equation to avoid dimensioned exponents:
is a total molar rate in kmol s⁻¹; earlier was a mass flux, so the overdot and A label matter. The source calls this rate . Both boundary fractions are recovered by Eq. 23. For , and .
Large Sh means a steep interfacial concentration gradient relative to the reference gradient across . Values of order one mean that reference diffusion scale is comparable. A stagnant sphere gives Sh two with diameter as , as derived below, rather than a universal value of one. For , and , . Using radius instead halves it; use the length required by the correlation. For a local coefficient use the matching local length; for a surface average use the average coefficient and the specified overall length. The convective topic derives these local and average forms.
For dilute A, . Compare the surface flux with to obtain
The leading two in sphere correlations is this diffusion limit, analogous to the heat-transfer limit. At concentrated A, Stefan flow increases the coefficient based on the simple concentration difference, so Sh equals two only for the stated dilute limit. Combining with the liquid balance
gives
in the infinite-film constant-property approximation. Diameter squared then decreases linearly. Real droplets can cool, encounter flow or change properties; those effects change the model. For a flowing gas, a suitable mass-transfer correlation accounts for the changed concentration field.
In steady spherically symmetric diffusion with no volumetric reaction, which quantity stays constant as radius increases?
Explanation
The same molar rate crosses every sphere surrounding the droplet:
Thus,
The area increases with the square of radius, so the local flux decreases as the inverse square. The total rate stays constant.
17 Additional examples
Section titled “17 Additional examples”Compare equimolar diffusion and a stagnant carrier
Section titled “Compare equimolar diffusion and a stagnant carrier”A binary ideal gas is at 300 K and 100 kPa. Across a 5.0 mm plane film, the mole fraction of A falls from 0.30 to zero. Use m² s⁻¹ and J mol⁻¹ K⁻¹. Compare the steady molar flux of A for equimolar counter-diffusion and for zero net flux of B. Take positive flux from the high-A face to the low-A face. Explain the difference and determine the flux ratio if the high-face mole fraction is reduced to 0.010, with all other data unchanged.
Solution
Data
| Quantity | Value |
|---|---|
| Temperature | |
| Pressure | |
| Film thickness | |
| Diffusivity | |
| Gas constant | |
| Side 1 mole fraction in the first comparison | |
| Side 2 mole fraction | |
| Side 1 mole fraction in the second comparison |
Assumptions
- Steady state.
- One-dimensional diffusion across a plane film.
- Ideal gas behaviour.
- Constant temperature, pressure and diffusivity.
- No reaction in the film.
Calculations
Positive flux points from the high-A face towards the low-A face. The total concentration is
For equimolar counter-diffusion, . As in Eq. 8, the bulk contribution vanishes and the governing relation is
Integrating between the film faces gives
For zero net flux of B, the total flux satisfies
Integrating this relation gives
A enters the film without a compensating net flux of B, producing molar flow in A’s direction. That bulk flow transports additional A. B still diffuses towards the high-A side, but its bulk contribution cancels its diffusion.
With , dividing the two fluxes gives
The common concentration, diffusivity and film thickness cancel. The ratios at the two supplied compositions are
As a dilute-limit check,
so the ratio approaches one as . The two models then give nearly the same flux.
Answer
At , the equimolar flux is and the stagnant-carrier flux is . The latter is 18.9 percent larger. At , their ratio falls to 1.005.
18 What you should now be able to calculate
Section titled “18 What you should now be able to calculate”Convert concentration and flux bases, distinguish equimolar from stagnant-carrier diffusion, and calculate plane or radial rates and slow interface motion.
Practice: Workshop 8 for evaporation and shrinking droplets.
19 Report an error
Section titled “19 Report an error”Email Ranjeet Utikar with the title
Fundamentals of mass diffusion, the URL /mass-transport/diffusion-fundamentals/, and the equation or passage to check.