Kaolinite, vermiculite, and montmorillonites were treated with solutions
containing hydroxy-chromium (OH-Cr) species. The OH-Cr solution was prepared
by adding 0·2 М NaOH to 0·1 М chromium nitrate solution
and allowing the solution to stand at 60°C for 1 day. The samples were
characterised by chemical analyses, N2
adsorption-desorption isotherms, and X-ray diffraction. The textural and
structural behaviours of kaolinite, vermiculite, and the montmorillonites were
analysed in the original samples and after treatment with the polymeric OH-Cr
species. The montmorillonites showed higher retention of chromium
(19·20%), higher basal spacing (2·06 nm), and higher
micropore surface area (276 m2/g) than the
vermiculite (3·70%, 1·49 nm, 13
m2/g) and kaolinite (1·15%,
0·73 nm, ~1 m2/g) clays after treatment
with the OH-Cr species. In contrast, the external surface area increased from
6 to 9 m2/g for kaolinite and from 18 to 24
m2/g for vermiculite, and decreased from 7 to 4
m2/g for montmorillonite after treatment with the
OH-Cr solution. The residual chromium, basal spacing, and texture of the clays
after treatment with the OH-Cr species were primarily related to the magnitude
of the negative charge originating from the octahedral sheet.