Interaction between n-butylammonium (BA) chloride and vermiculite from Sant
a Olalla (Spain) has been studied in large flake (5 x 5 x 0.1 mm) or ground
powder (less than or equal to 80 mu m) samples. The differences in adsorpt
ion and decomposition of BA ions in both particle sizes have been establish
ed. In the interlamellar space, the BA ion remains unaltered in powder samp
les, but is degraded in flakes. The experimental results suggest decomposit
ion of the BA in the interlamellar space of vermiculite flakes by breaking
of the C-N bond. The degradation of BA takes place over a short period. The
variety with BA in the interlamellar space is transformed into a new one,
due to the degradation of alkylammonium. The transformation occurs through
an interstratified phase formed between BA-vermiculite and NH4-vermiculite,
and finally a phase appears in which only ammonium is present in the inter
lamellar space. Due to the many industrial applications of alkylammonium-cl
ays, determination of the stability of alkylammonium in the interlamellar s
pace of clay minerals is of great importance.