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LANGMUIR ADSORPTION ISOTHERM      41

                               Type I       Type II     Type III




                         Q
                                         B



                                 P    P°      P    P°     P     P°
                                     Type IV      Type V




                               Q





                                       P     P°     P    P°
            Figure 4.1  The five types of adsorption isotherms according to the classification of
            Brunauer (1945).




              One notes with interest the similarity in shape of type III adsorption
            isotherm and a special partition isotherm, as depicted in Figure 3.2, when a
            solute partitions very favorably from water (or other media) into an organic
            phase (or solvent). Whereas the isotherm in Figure 3.2 is for the solute par-
            tition from water into an organic phase, a similar partition isotherm arises
            when the vapor of a liquid partitions strongly into an organic substance. Illus-
            trative examples of such a vapor partition phenomenon are benzene, toluene,
            xylene, and carbon tetrachloride on rubber, polystyrene, and polyiosbutylene
            (Eichinger and Flory, 1968a,b). A practical means to distinguish a type III
            vapor adsorption isotherm from a similarly shaped vapor partition isotherm
            is that the vapor partition should display a very high uptake capacity, usually
            more than 10% by weight at P/P° = 0.5, while a type III vapor adsorption
            exhibits a very low capacity, usually far less than 1% by weight, at P/P° = 0.5.



            4.2 LANGMUIR ADSORPTION ISOTHERM

            Langmuir (1918) considered the adsorption of gases or vapors on a plane
            surface that contains a fixed number of identical active sites. From a kinetic
            consideration, the rate of vapor desorption from the occupied sites is set equal
            to the rate of adsorption on the unoccupied sites at equilibrium:
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