Page 260 - Adsorption by Powders and Porous Solids
P. 260

248                            ADSORPTION  BY POWDERS AND POROUS SOms

       The energetic heterogeneity of the original ungraphitized surface was revealed by
     the careful adsorption calorimetric measurements undertaken by Beebe et al., (1953).
     By comparing the changes in the differential energies of  adsorption for argon on
     Spheron and Graphon, these investigators found that the initial steep decline in 'dif-
     ferential  heat  of  adsorption'  was largely removed  as a  result  of  graphitization.
     Instead, an increase in the differential energy was observed at a higher surface cov-
     erage: it is now generally agreed that this was due to the adsorbate-adsorbate inter-
     action becoming apparent as the degree of energetic heterogeneity was reduced.
       A systematic study of laypton adsorption on exfoliated graphite was subsequently
     undertaken  by  Thomy  and  co-workers (Thorny  and  Duval,  1969; Thorny  et a!.,
      1972). Their stepwise isotherm, determined at 77.3 K, is shown in Figure 4.1. The
     layer-by-layer nature of the physisorption process is clearly evident - at least up to
     four  molecular  layers.  This  isotherm shape is  remarkably  similar to  that  of  the
     krypton isotherm on graphitized carbon black reported by Arnberg er al., (1955).
       The work of Thorny and co-workers (Thorny and Duval, 1969; Thorny et al., 1972)
     provided the first well-documented evidence for the presence of  a sub-step in the
     krypton isotherm. The effect of temperature on the shape and the location of the sub-
      step is shown in Figure 9.7. The fact that the riser of the sub-step remained vertical
     over the temperature range of 77.3-96.3 K served to confirm that the sub-step was

































      Figure 9.7.  Adsorption isotherms of krypton on exfoliated graphite. Curves labelled from  1 to  10,
      obtained at 77.3, 82.4, 84.1,85.7,86.5,87.1,  88.3.89.0.90.1  and 90.9 K, respectively (courtesy Thorny
      eta[., 1972).
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