Page 120 - Adsorption by Powders and Porous Solids
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,-wTER  4. INTERPRETATION OF PHYSISORPTION ISOTHERMS           105







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                                                        LIQUID + SOLID


















          Figure 4.2.  Adsorption isotherms of xenon on FeC1,  (courtesy of Larher, 1992).


    was displayed up to four molecular layers, as can be seen in Figure 4.1. Each vertical
    'riser' (at constantp/po) can be regarded as a phase transition between one adsorbed
    layer and the next higher layer.
      In the sub-monolayer range, three distinctive regions were identified and attributed
    by  Thomy and Duval to 2-D 'gas', 'liquid' and 'solid'  phases. These measurements
    provided the first unambiguous evidence for the existence of sub-steps in the mono-
    layer region of a stepwise, Type VI, isotherm.
      To illustrate the interpretation of such sub-steps, the monolayer isotherms for the
    adsorption of Xe on FeC1,  (Larher, 1992) are shown in Figure 4.2.  At temperatures
    below 99.57 K, there is a single vertical step, which corresponds to the transforma-
    tion of 2-D gas to the solid phase. Very little further compression of the monolayer is
    possible before its completion at Point B. A smaller sub-step becomes apparent at
    temperatures above 99.57 K. As a result of the careful studies of Thomy and Duval
    and Larher, the consensus interpretation is that this small sub-step represents a first-
    order transition between the 2-D liquid and solid phases. It is evident that, in the case
    of the Xe/FeCl,  system, 99.57 K is the two-dimensional triple point.
      Two-dimensional phase diagrams are often displayed in the form of In [p] against
     1/T (at a constant specific amount adsorbed), which provides a convenient way of
    indicating the conditions for the coexistence of two phases (see Figure 4.3). Indeed,
    the application of  the Phase Rule indicates that when two adsorbed phases coexist
    in  equilibrium,  the  system  has  one  degree  of  freedom:  therefore,  at  constant
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