Adsorption-desorption of simazine on model systems which closely simulate t
hose encountered in soils [i.e., pure montmorillonite and montmorillonite c
overed by different amounts of OH-Al species (chlorite-like complexes)] was
investigated. The adsorption date were analyzed according to Langmuir and
Freundlich equations. Results obtained indicate that the adsorption of sima
zine was strongly influenced by the charge characteristics of clay minerals
and the pH of buffer (3.7 and 5.6). At pH 3.7, simazine was adsorbed in la
rge amounts on montmorillonite, whereas adsorption significantly decreased
with increasing amounts of Al(OH)(x) species on montmorillonite surfaces. W
hen experiments were carried out at pH 5.6, the adsorption of the herbicide
an montmorillonite drastically decreased, whereas no severe differences we
re observed with AM(18) (a montmorillonite loading 18 mequiv g(-1) M). Deso
rption tests showed that negligible and very little amounts of simazine wer
e desorbed from montmorillonite and AM(18), respectively. Strong electrosta
tic interactions were involved in the adsorption process. Simazine molecule
s, arriving at support interfaces mostly as molecular species, dissociated
as cations by the microenvironmental pH ("surface acidity") and were adsorb
ed by cation-exchange mechanism.