As a model of chemical soil contamination, adsorption of aniline and p
-nitrophenol onto Ca-bentonite at different pH has been studied. At pH
around the value corresponding to pK(s) aniline is adsorbed to the ma
ximal extent of almost-equal-to 15%. So we may conclude that this cont
aminant is mainly adsorbed by ion exchange as aniline cation. Desorpti
on or soil decontamination may be achieved by HCl or NaOH to almost-eq
ual-to 30% under clay destruction; however, through ion re-exchange wi
th an excess amount of CaCl2, 100% of aniline is desorbed. Alternative
ly, aniline may be removed from bentonite by oxidation in air at 250 t
o 400-degrees-C. Nitrophenol is only very weakly adsorbed at any measu
red pH.