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REFERENCES 187
A note needs to be made about the interactions with zeolites that have diva-
lent (and higher valent) cations. The interaction energies of CO 2 with X zeo-
lites that have different univalent cations follow the order that larger ions give
lower heats of adsorption (Table 7.4 above, and Barrer, 1978). For divalent
ions, the heats follow the reverse order of Ba 2+ > Sr 2+ > Ca 2+ (Barrer, 1978).
This is also the case for N 2 adsorption on zeolites with different univalent
and divalent cations (Mckee, 1964). Both N 2 and CO 2 are nonpolar but highly
quadrupolar. For adsorption on zeolites exchanged with univalent cations, the
term dominates. With divalent cations, however, the large polarizabili-
φ ˙ FQ
ties (Table 2.2) become important, and the dispersion and induction energies
are significantly large, especially for Ba . Hence all interaction terms need to
2+
be considered.
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