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9.3 Representation of equilibrium  247




               The simplest adsorption isotherm expresses loading (q) as proportional to fluid phase concentration,
                                      resulting in an expression similar to Henry’s law.

                                                               q ¼ b   c                     (9.5)
                    Isotherm equations
                                      c is the equilibrium concentration of the solute in the mixture.

                                         There are three commonly used mathematical expressions e
               Langmuir, BET (BrunauereEmmetteTeller), and Freundlich isotherms to describe vapor/gas
               adsorption equilibria as q vs p , the equilibrium partial pressure.

                  Table 9.4 provides the details of the equations.


                 Table 9.4 Vapor/Gas-solid adsorption isotherms.
                                                         Assumptions/
                 Isotherm     Corresponding equation    Considerations         Special features
                 Langmuir  q ¼ b 1   p =ð1 þ b 2   p Þ  Accounts for surface


                 isotherm  b 1 e Slope of the isotherm  coverage, i.e., for high
                           at zero coverage (Henry’s  fluid concentration,
                           law coefficient)           adsorbate monolayer
                           b 2 e Constant            forms on the adsorbent
                           p e equilibrium pressure of  surface

                           the solute
                 BET              1                  Multilayer adsorption  · linear in the range
                 equation        sat     ¼           theory based on       0.05 < ð p sat  = p Þ < 0.35

                            q  ½ð p =p Þ  1Š
                                                     Langmuir model      · not applicable for
                            k   1   p      1


                           q m   k     p sat  þ q m   k                    supercritical conditions
                                                                         · seldom used for data
                                                                           correlation and representation
                           q m e loading corresponding
                           to complete monolayer
                           adsorption
                           k e BET equation constant
                           p sat  e Saturation pressure of the
                           solute
                                       K c
                 Freundlich  q ¼ K F  ð p Þ          Empirical fitting of  · most commonly used
                 isotherm  K F , K c   - constants for each  isotherm data to a linear  isotherm, although the
                                                     equation in log-log   equation is
                           solute-adsorbent pair at a fixed
                                                     coordinates           thermodynamically
                           temperature
                                                                           inconsistent
                           K F depends on nature of
                                                                         · works well for heterogeneous
                           adsorbent and adsorbate                         surfaces
                                                                         · limited application range as it
                                                                           does not describe isotherm
                                                                           over a wide range of pressure
                 Timken    q ¼ b 1 ln K T þ b 1 ln c ,                   Chemical bonding with

                 isotherm  K T ,b 1 e constants                          adsorbate
                 While Langmuir isotherm is theoretically justified, Freundlich isotherm is of a purely empirical character since it does not have
                a finite Henry’s law constant.
                  As is evident from equation, Freundlich isotherms are linear for K c ¼ 1, concave upward for K c > 1 and concave downward for
                K c < 1. Generally 2 < K c > 10 represents good and 1 < K c > 2 represents moderately difficult adsorption characteristics. K c < 1
                depicts poor adsorption characteristics and requires impractically large adsorption dosage for appreciable solute removal.
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