Page 64 - Gas Adsorption Equilibria
P. 64

50                                                         Chapter 1


          curves are characteristic for the hydrophilic behavior of the zeolites reflected
          in the  steep  increase  of the respective isotherms at very low (relative) vapor
          pressures, this indicating  existence of micropores. The curves also  show for
          activated  carbon  hydrophobicity and for activated  alumina, amphoteric
          behavior. For  adsorption based  air conditioning  systems the  isotherms of
          silica gel and activated alumina H-151  are most advantageous, allowing one
          to operate the process in a wide range of pressure          with fairly
          large amounts of water vapor to be either adsorbed or desorbed upon pressure
          increase or decrease in this region.


























          Figure 1.17. Adsorption isotherms of  water  vapor on  different  porous materials  taken at
                    T = 25  °C, the saturation pressure being  Reprint  taken  from  [1.39]
                    with permission granted.

             Gas adsorption systems  normally  do not only  differ in  their adsorption
          capacity, i.  e.  thermodynamic equilibria states, but  also in  their kinetic
          behavior, i.  e.  spontaneity  of  uptake or  release of  gas  upon increase or
          decrease of sorptive gas pressure. Examples for this are given in Figures 1.18,
          1.19,  showing the  uptake  process of carbon dioxide  (4.5))  on  dry Fig.
          (1.18), and prewetted, Fig. (1.19) zeolite molecular sieve MS Na 13X (Linde,
          UOP)  at  T = 323 K due to an  increase of the sorptive  gas  pressure  from
          0.5 MPa to 6 MPa, [1.60].

             In both Figures the uptake  of  (upper curves) and the gas temperature
          (lower curve),  measured immediately  below the microbalance  connected
          sorbent sample are shown as functions of time, approaching equilibrium after
          ca. 5 hours.  For the  dry zeolite experiment an overshooting of the uptake of
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