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HORV ´ ATH–KAWAZOE APPROACH  73

            estimates the pore size of the material as 45 ˚ A. By using the same model
            parameters (shown in Table 4.2), the original HK and HK–CY models give a
            grossly underestimated pore size of 12 ˚ Aand 9 ˚ A, respectively. It must be noted
            that the corrected HK equation without the Cheng–Yang correction gives a highly
            overestimated pore size value (beyond the limits of Fig. 4.9). This is because the
            inflexion in the curve occurs at a high P/P S value (∼0.4). There is a severe
            deviation from Henry’s law at this value. Further, Ravikovitch et al. (1997) have
            reported that the BJH method systematically underestimated the pore size of the
            MCM-41 materials studies by ∼10 ˚ A. Thus, the utility of the corrected HK–CY
            model in predicting PSD for materials in the mesoporous (>20 ˚ A) size range is
            demonstrated.
              Like zeolitic materials, aluminophosphates also possess well-defined structure
            and narrow PSD. Most aluminophosphates such as AlPO 4 -11 and VPI-5 have
            a one-dimensional channel structure. Adsorption isotherms of argon on these
            materials have been reported by Davis et al. (1988).
              Figure 4.10 shows the computed PSD of VPI-5 aluminophosphate whose
            isotherm is seen to have two sigmoidal bends, suggesting that it may have a
            bimodal PSD. The currently accepted pore size of VPI-5 is 12.1 ˚ A(Daviset al.,
            1988). It was shown previously by Cheng and Yang (1994) that VPI-5 gives two
            peaks by use of the original HK–CY equation: a major peak at 8.6 ˚ Aand a
            minor one at 11.7 ˚ A. In the work of Rege and Yang (2000) different parameters
            were used for the kinetic diameter of argon and the oxide ion density in the
            aluminophosphate framework. As a result the new peaks obtained by using the
            original model were situated at 6.8 ˚ A and at 8.7 ˚ A. With the modified HK–CY
            model the major peak was observed at 11.8 ˚ A and a minor peak was observed



                                                     Original HK
                         3.0                         Original HK–CY
                                                     Corrected HK
                         2.5
                                                     Corrected HK–CY
                         2.0
                        d(W/W 0 )/dL  1.5



                         1.0

                         0.5

                         0.0
                            4     6    8    10    12   14    16   18
                                       Effective channel size (Å)
            Figure 4.10. Pore size distribution of VPI-5 as predicted by original HK models and the
            corrected HK models for cylindrical pores (Rege and Yang, 2000, with permission).
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