Gy. Sheng et al., SURFACE HETEROGENEITY OF TRIMETHYLPHENYLAMMONIUM-SMECTITE AS REVEALEDBY ADSORPTION OF AROMATIC-HYDROCARBONS FROM WATER, Clays and clay minerals, 45(5), 1997, pp. 659-669
Adsorption studies of aromatic hydrocarbons of various molecular sizes
on organoclays in aqueous solution were carried out for characterizin
g the surface heterogeneity of organo-clays. Benzene, toluene, p-xylen
e, ethylbenzene and n-propylbenzene adsorption by a smectite with 5 di
fferent exchange degrees of trimethylphenylammonium (TMPA) cations for
Ca2+ was measured. The Langmuir isotherm equation did not adequately
describe the experimental data, especially for small molecules, wherea
s the Dubinin-Radushkevich (DR) equation combined with a gamma-type ad
sorption energy distribution function described all experimental data
well, suggesting the surface and structural heterogeneity of TMPA-smec
tites. The calculated adsorption energy distributions indicated that t
he apparent heterogeneity depends on the molecular size of adsorbates.
Small adsorbate molecules such as benzene explore a highly heterogene
ous surface of TMPA-smectites while large molecules such as n-propylbe
nzene detect a relatively homogeneous surface. The surface fractal dim
ension was dependent on the extent of TMPA exchange for Ca2+. When TMP
A content is less than 75% of the cation exchange capacity (CEC) of th
e smectite, the heterogeneity decreases as TMPA content increases; it
increases with TMPA content thereafter: These results are related to t
he size distribution of micropores in TMPA-smectites, which are define
d by the 2 semi-infinite aluminosilicate sheets and the interlayer cat
ions. The micropore size distributions and, hence, heterogeneity are c
reated in part by the inhomogeneity of the charge density of clay surf
aces and the tendency for cation segregation in these systems.