DIFFUSION
CHEMICAL ENGINEERING REVIEW
PRINCIPLES OF DIFFUSION
MASS TRANSFER
Is the net movement of a component in a mixture from one location to another location where the component exists at a different concentration
The transfer takes place between the two phases across an interface
Mass transfer occurs by two basic mechanisms: (1) molecular diffusion and (2) eddy diffusion
MOLECULAR DIFFUSION
Transfer or movement of individual molecules through a fluid by means of the random, individual movements of the molecules
In a binary mixture, molecular diffusion occurs because of one or more different potentials or driving forces
1. Concentration gradient (ORDINARY DIFFFUSION) 2. Pressure gradient (PRESSURE DIFFUSION) 3. Temperature (THERMAL DIFFUSION)
4. External force fields (FORCED DIFFUSION) as in centrifuge 5. Activity gradient as in reverse osmosis
Molecular diffusion occurs in solids and in fluids that are stagnant or in laminar or turbulent motion
EDDY (TURBULENT) DIFFUSION
Takes place in fluid phases by physical mixing and by the eddies of turbulent flow
FICK’S LAW OF DIFFUSION AT STEADY STATE Fick’s Law of Diffusion
Gives the rate of mass transfer by molecular diffusion perpendicular to an relative to a stationary surface which is at fixed distance from the interface
Fick’s First Law of Molecular Diffusion is proportionality between a flux and a gradient. For a
binary mixture of A and B
𝑟𝑎𝑡𝑒 𝑜𝑓 𝑡𝑟𝑎𝑛𝑠𝑓𝑒𝑟 𝑝𝑟𝑜𝑐𝑒𝑠𝑠 = 𝑑𝑟𝑖𝑣𝑖𝑛𝑔 𝑓𝑜𝑟𝑐𝑒 𝑟𝑒𝑠𝑖𝑠𝑡𝑎𝑛𝑐𝑒 𝜓𝑧 = −𝛿
𝑑Γ 𝑑𝑧
𝐽𝐴𝑥 = 𝑁𝐴 𝐴 = −𝐷𝐴𝐵 𝑑𝐶𝐴 𝑑𝑍 and 𝐽𝐵𝑥 = 𝑁𝐵 𝐴 = −𝐷𝐵𝐴 𝑑𝐶𝐵 𝑑𝑍 where:
𝐽𝐴𝑥 - is the molar flux of A by ordinary molecular diffusion relative to the molar average velocity of the mixture in the positive z direction
𝐷𝐴𝐵 - mutual diffusion coefficient of A and B 𝑑𝐶𝐴
𝑑𝑥
⁄ - concentration gradient of A, which is negative in the direction of ordinary molecular diffusion 𝑁𝐴 - moles of A diffusing per unit time
𝐴 - cross sectional area 𝐶𝐴 - concentration of A
𝑍 - distance of diffusion
Fick’s Law of diffusion is based on the following observations:
1. Mass transfer by ordinary molecular diffusion occurs because of a concentration difference or gradient; that is, a species diffuses in the direction of decreasing concentration
2. The mass transfer rate is proportional to the area normal to the direction of mass transfer and not to the volume of the mixture. Thus, the rate can be expressed as a flux
3. Mass transfer stops when the concentration is uniform
PREDICTION OF DIFFUSIVITY For Gases:
1. Chapman and Enskog Equation 𝐷𝐴𝐵 = 1.8583 𝑥 10−7 𝑇3/2 𝑃𝜎𝐴𝐵2Ω𝐷,𝐴𝐵 ( 1 𝑀𝐴 + 1 𝑀𝐵 ) 1/2 Where: 𝐷𝐴𝐵 – diffusivity, m2/s 𝑇 - temperature, K
𝑃 – absolute pressure, atm
𝑀𝐴, 𝑀𝐵 - molecular weights of A and B, in kg/kmol 𝜎𝐴𝐵 - average collision diameter, Å
𝛺𝐷,𝐴𝐵 - collision integral based on the Lennard-Jones potential
2. Fuller Method (Geankoplis) 𝐷𝐴𝐵= 1 𝑥 10−7 𝑇1.75 𝑃[(∑ 𝑢𝐴)1/3+ (∑ 𝑢𝐵)1/3]2 ( 1 𝑀𝐴 + 1 𝑀𝐵 ) 1/2 Where:
∑ 𝑢𝑖 - sum of structural volume increments (table 6.2-2, Geankoplis) 3. Schmidt Number 𝑆𝑐 = 𝜇 𝜌𝐷𝐴𝐵 For liquids: 1. Stokes-Einstein Equation 𝐷𝐴𝐵 = 7.32 𝑥 10−16 𝑇 𝑟𝑜𝜇 Where: 𝐷𝐴𝐵 - diffusivity, cm2/s 𝑇 - absolute temperature, K 𝑟𝑜 - molecular radius, cm 𝜇 - viscosity, cP 2. Wilke-Chang Equation 𝐷𝐴𝐵 = 7.4 𝑥 10−8 (𝜓𝐵𝑀𝐵)1/2𝑇 𝜇𝑉𝐴0.6 Where:
𝑉𝐴 - molar volume of solute as liquid at its normal boiling point, cm3/mol
𝜓𝐵- association parameter for solvent (water = 2.6; methanol = 1.9; ethanol = 1.5; benzene = 1.0; heptanes = 1.0)
3. Nernst Equation (for dilute solutions of completely ionized univalent electrolytes 𝐷𝐴𝐵 = 2𝑅𝑇 (1 𝜆+0 + 1 𝜆0−) 𝐹𝑎 2 Where:
𝐹𝑎 - Faraday constant, 96,500 coul/gequiv 𝑅 - gas constant, 8.314 J/K·gmol
𝜆0+, 𝜆−0 - limiting (zero concentration) ionic conductances, A/cm2·(V/cm)·(gequiv/cm3), Table 17.1 Unit Operations by McCabe and Smith
MOLECULAR DIFFUSION IN GASES
1. EQUIMOLAR COUNTER-DIFFUSION
𝐽
∗ 𝐴= −𝐽
∗𝐵𝐽
𝐴∗=
𝑁
𝐴𝐴
= −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑍
𝐶
𝐴=
𝑛
𝐴𝑉
=
𝑝
𝐴𝑅𝑇
𝐽
𝐴∗= −
𝐷
𝐴𝐵𝑅𝑇
𝑑𝑝
𝐴𝑑𝑍
Where:
𝐽
𝐴∗- diffusion flux relative to the moving fluid
2. GENERAL CASE FOR DIFFUSION OF GASES A AND B PLUS CONVECTION
In terms of velocity of diffusion of A to the right
𝐽
𝐴∗= 𝑢
𝐴𝑑𝐶
𝐴If the whole fluid is moving in bulk or convective to the right
𝑢
𝐴= 𝑢
𝐴𝑑+ 𝑢
𝑀𝐶
𝐴𝑢
𝐴= 𝐶
𝐴𝑢
𝐴𝑑+ 𝐶
𝐴𝑢
𝑀𝐽
𝐴= 𝐽
𝐴∗+ 𝐶
𝐴𝑢
𝑀Let 𝑁 = total convective flux of the whole stream, relative to the stationary point, then
𝐽 = 𝐶𝑢
𝑀= 𝐽
𝐴+ 𝐽
𝐵𝑢
𝑀=
𝐽
𝐴+ 𝐽
𝐵𝐶
𝐽
𝐴= 𝐽
𝐴∗+
𝐶
𝐴𝐽
𝐴= −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑍
+
𝐶
𝐴𝐶
(𝐽
𝐴+ 𝐽
𝐵)
For equimolar counter-diffusion,
𝐽
𝐴= −𝐽
𝐵𝐽
𝐴=
𝑁
𝐴𝐴
= −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑍
= −
𝐷
𝐴𝐵𝑅𝑇
𝑑𝑝
𝐴𝑑𝑍
3. SPECIAL CASE FOR A DIFFUSING THROUGH STAGNANT, NON-DIFFUSING B
In this case,
𝐽
𝐵= 0
𝐽
𝐴= −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑍
+
𝐶
𝐴𝐶
𝐽
𝐴𝐽
𝐴(1 −
𝐶
𝐴𝐶
) = −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑍
𝐽
𝐴(
𝐶 − 𝐶
𝐴𝐶
) = −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑍
𝐽
𝐴[
𝑃
𝑅𝑇 −
𝑝
𝐴𝑅𝑇
𝑃
𝑅𝑇
] = −
𝐷
𝐴𝐵𝑅𝑇
𝑑𝑝
𝐴𝑑𝑍
𝐽
𝐴(
𝑃 − 𝑝
𝐴𝑃
) = −
𝐷
𝐴𝐵𝑅𝑇
𝑑𝑝
𝐴𝑑𝑍
𝐽
𝐴=
𝑁
𝐴𝐴
= −
𝐷
𝐴𝐵𝑃
𝑅𝑇
(
1
𝑃 − 𝑝
𝐴)
𝑑𝑝
𝐴𝑑𝑍
MOLECULAR DIFFUSION IN LIQUIDS
4. EQUIMOLAR COUNTER-DIFFUSION
𝐽
𝐴=
𝑁
𝐴𝐴
= −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑧
𝐶
𝐴= 𝐶
𝑎𝑣𝑥
𝐴𝐶
𝑎𝑣= (
𝜌
𝑀
)
𝑎𝑣=
1
2
(
𝜌
1𝑀
1+
𝜌
2𝑀
2)
Where:
𝐶
𝑎𝑣- average total concentration of liquids A and B, mol/vol
𝑥
𝐴- mol fraction of A
5. DIFFUSION OF A THROUGH A NON-DIFFUSING B
𝐽
𝐴= −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑧
+
𝐶
𝐴𝐶
𝑎𝑣(𝐽
𝐴+ 𝐽
𝐵)
𝐽
𝐵= 0
𝐽
𝐴=
𝑁
𝐴𝐴
= −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑧
+
𝐶
𝐴𝐶
𝑎𝑣𝐽
𝐴𝐽
𝐴(1 +
𝐶
𝐴𝐶
𝑎𝑣) = −𝐷
𝐴𝐵𝑑𝐶
𝐴𝑑𝑧
𝐶
𝐴= 𝐶
𝑎𝑣𝑥
𝐴𝑑𝐶
𝐴= 𝐶
𝑎𝑣𝑑𝑥
𝐴𝐽
𝐴(1 + 𝑥
𝐴) = −𝐷
𝐴𝐵𝐶
𝑎𝑣𝑑𝑥
𝐴𝑑𝑧
𝐽
𝐴∫ 𝑑𝑧
𝑍2 𝑍1= −𝐷
𝐴𝐵𝐶
𝑎𝑣∫
𝑑𝑥
𝐴1 + 𝑥
𝐴 𝑥𝐴2 𝑥𝐴1𝐽
𝐴(𝑍
2− 𝑍
1) = −𝐷
𝐴𝐵𝐶
𝑎𝑣ln
1 + 𝑥
𝐴21 + 𝑥
𝐴1𝐽
𝐴=
𝑁
𝐴𝐴
=
−𝐷
𝐴𝐵𝐶
𝑎𝑣(𝑍
2− 𝑍
1)
ln
1 + 𝑥
𝐴21 + 𝑥
𝐴1𝑥
𝑙𝑚=
(𝑥
𝐴1− 𝑥
𝐵1) − (𝑥
𝐴2− 𝑥
𝐵2)
ln
𝑥
𝑥
𝐴1− 𝑥
𝐵1 𝐴2− 𝑥
𝐵2For dilute solution,
𝑥
𝐴≪≪ 𝑥
𝐵𝑥
𝑙𝑚=
(0 − 𝑥
𝐵1) − (0 − 𝑥
𝐵2)
ln
0 − 𝑥
0 − 𝑥
𝐵1 𝐵2𝑥
𝑙𝑚=
𝑥
𝐵2− 𝑥
𝐵1ln
𝑥
𝑥
𝐵2 𝐵1ln
𝑥
𝐵2𝑥
𝐵1=
𝑥
𝐵2− 𝑥
𝐵1𝑥
𝑙𝑚𝐽
𝐴=
𝑁
𝐴𝐴
=
−𝐷
𝐴𝐵𝐶
𝑎𝑣(𝑍
2− 𝑍
1)
ln
1 + 𝑥
𝐴21 + 𝑥
𝐴1𝐽
𝐴=
𝑁
𝐴𝐴
=
−𝐷
𝐴𝐵𝐶
𝑎𝑣(𝑍
2− 𝑍
1)
ln
𝑥
𝐵2𝑥
𝐵1𝐽
𝐴=
𝑁
𝐴𝐴
=
−𝐷
𝐴𝐵𝐶
𝑎𝑣(𝑍
2− 𝑍
1)
(
𝑥
𝐵2− 𝑥
𝐵1𝑥
𝑙𝑚)
For dilute solutions,
𝑥
𝑙𝑚= 1
𝐽
𝐴=
𝑁
𝐴𝐴
= −
𝐷
𝐴𝐵𝐶
𝑎𝑣(𝑍
2− 𝑍
1)
(𝑥
𝐵2− 𝑥
𝐵1)
𝐽
𝐴=
𝑁
𝐴𝐴
= −
𝐷
𝐴𝐵𝐶
𝑎𝑣(𝑍
2− 𝑍
1)
(𝑥
𝐴2− 𝑥
𝐴1)
𝐽
𝐴=
𝑁
𝐴𝐴
= −𝐷
𝐴𝐵𝐶
𝑎𝑣(𝑥
𝐴2− 𝑥
𝐴1)
(𝑍
2− 𝑍
1)
= −𝐷
𝐴𝐵(𝐶
𝐴2− 𝐶
𝐴1)
(𝑍
2− 𝑍
1)
MOLECULAR DIFFUSION IN SOLIDS
𝑱
𝑨=
𝑵
𝑨𝑨
= −𝑫
𝑨𝑩𝒅𝑪
𝑨𝒅𝒛
6. DIFFUSION EQUATIONS USING GAS SOLUBILITY IN A SOLID SURFACE
𝐶
𝐴=
𝑆𝑝
𝐴𝑉̅
Where: 𝑉̅ is the molar volume of gas at STP, 22.4 m
3/kmol; 𝑆 – solubility of solute
gas in a solid
7. DIFFUSION IN SOLIDS USING PERMEABILITY EQUATIONS
𝑃
𝑀= 𝐷
𝐴𝐵𝑆
Where: 𝑃
𝑀- solute gas permeability, or the volume of solute gas at STP diffusing per
second per unit cross sectional area through a solid under a pressure difference of 1
atm pressure
8. DIFFUSION IN POROUS SOLIDS THAT DEPENDS ON STRUCTURE
𝐽
𝐴=
𝑁
𝐴𝐴
=
𝜀𝐷
𝐴𝐵(𝐶
𝐴1− 𝐶
𝐴2)
𝜏(𝑍
2− 𝑍
1)
Where:
𝜀 - open void fraction; 𝜏 -
tortousity (factor that corrects for
the path longer than the (𝑍
2− 𝑍
1)
MASS TRANSFER COEFFICIENTS
MASS TRANSFER COEFFICIENT
It is defined as the rate of mass transfer per unit area per unit concentration difference
and is usually based on equal molal flows
𝑘
𝐶=
𝐽
𝐴𝐶
𝐴𝑖− 𝐶
𝐴𝑘
𝑦=
𝐽
𝐴𝑦
𝐴𝑖− 𝑦
𝐴𝑘
𝐶= [
𝐷
𝐴𝐵(𝐶
𝐴𝑖− 𝐶
𝐴)
𝑍
2− 𝑍
1] (
1
𝐶
𝐴𝑖− 𝐶
𝐴) =
𝐷
𝐴𝐵∆𝑍
Sherwood Number
𝑆ℎ =
𝑘
𝐶𝐷
𝐷
𝐴𝐵Reynold’s Number
𝑅𝑒 =
𝐷𝑢𝜌
𝜇
=
𝐷𝐺
𝜇
Graetz Number
𝐺𝑧 =
𝑚̇
𝐷
𝐴𝐵𝐿𝜌
Schmidt Number
𝑆𝑐 =
𝜇
𝜌𝐷
𝐴𝐵Peclet Number
𝑃𝑒 = 𝑅𝑒 𝑥 𝑆𝑐
MASS TRANSFER WITH FLOW INSIDE PIPES
- Prediction of the internal mass-transfer resistance for separation processes using
hollow-fiber membranes
𝑆ℎ = 1.62𝐺𝑧
1/3- For turbulent flow mass transfer to pipe walls
𝑆ℎ = 0.023 𝑅𝑒
0.8𝑆𝑐
1/3(
𝜇
𝜇
𝑤𝑎𝑙𝑙)
0.14