Introduction
Surface processes of modest size aromatic molecules
on clay matrices have been of massive interest for elu-
cidating the chemical reactivity and mechanical prop-
erties of organo-clay composites [1–3]. The
organo-clay composites which possess large specific
surface area, considerable porosity and thermal stabil-
ity have been widely used in a range of key processes
as ion exchangers, selective adsorbents and reinforc-
ing fillers for plastics and electric materials [4–6].
The host centres produced by immobilization of spe-
cific guest molecules such as formamide, urea and
short chain oil acids through strong hydrogen bonds
into the inorganic matrices such as kaolinite are of
great importance in catalyis [7–10]. Organic and inor-
ganic molecules may form ‘intercalation compounds’
within the unique structure of kaolinite by overcom-
ing the cohesive forces between free surface hydroxyl
groups [11] whereas non-reacting molecules of large
size are entrained by the precursors such as DMSO
and NMF [7, 12]. Considerable attention has been
paid to characterize the precursors to ordered org-
ano-clay composites formed on kaolinite-type miner-
als [13–15].
The benzamide species retained by pre-adsorbed
DMSO composites at a kaolinite surface which
should represent a clear possibility of new and prom-
ising materials were examined in present work
through the use of FTIR, thermal analysis (TG-DTG
and DTA), X-ray powder diffraction (XRD) and sur-
face area measurement techniques.
Experimental
XRD pattern of the kaolinite (K, Sigma, 212 mm)
showed no crystalline impurities. DMSO [Fluka,
99.9%, (G.C.)] and benzamide (Fluka, ³98% (UV))
were used as received. 3 g K was mechanically stirred
with 40 mL DMSO at 60°C for 2 days in a 50-mL
flat-bottomed glass flask and the resulting kao-
linite-dimethyl sulphoxide (K-DMSO) composite
was washed with ethanol two times; the supernatant
solution was centrifuged at 2000 rpm and the solid
product was dried for 2 days at 60°C to eliminate the
excess of DMSO [13, 14]. The displacement tech-
nique (from the K-DMSO composite) was used to
prepare the kaolinite-benzamide (K-Bz) intercalate.
1 g K-DMSO was thoroughly mixed with excess
benzamide aqueous solution for 5 days at 130°C. The
supernatant was discarded and the product washed
twice with ethanol and subsequently by hot water.
The solid product was dried for 2 days at 80°C and
then sieved to 212 mm [9].
XRD profiles were recorded on a Rigaku 2000
instrument using Ni-filtered CuK
a
radiation (l,
1.54050 ) at 40 kV and 40 mA. Infrared spectra
were collected in the 4000–200 cm
–1
region with
Mattson-1000 FTIR spectrometer at 4 cm
–1
resolution
using KBr pellet technique.
Simultaneous TG-DTG and DTA curves were
monitored using Rigaku TG 8110 analyser equipped
with TAS 100 from room temperature to 1000°C at a
heating rate of 10°C min
–1
under nitrogen flow
(calcinated a-alumina was taken as the reference).
Surface areas were measured by nitrogen adsorption
at 77 K using Quantachromosorb.
1388–6150/$20.00 Akadémiai Kiadó, Budapest, Hungary
© 2007 Akadémiai Kiadó, Budapest Springer, Dordrecht, The Netherlands
Journal of Thermal Analysis and Calorimetry, Vol. 87 (2007) 2, 429–432
BENZAMIDE SPECIES RETAINED BY DMSO COMPOSITES AT A
KAOLINITE SURFACE
B. Caglar, B. Afsin
*
and A. Tabak
Department of Chemistry, Faculty of Arts and Sciences, Ondokuz Mayis University, Kurupelit, Samsun, 55139 Turkey
The surface area of kaolinite-benzamide (K-Bz) 6.62 m
2
g
–1
, which is noticeably lower than that of kaolinite-dimethyl sulphoxide
(K-DMSO) 14.61 m
2
g
–1
, the co-perturbation of the inner-surface hydroxyl features at 3697 and 3650 cm
–1
, and the increase of d(001)
value by 7.44 are all related to the benzamide species inserted into the kaolinite structure through the replacement of the K-DMSO
composites. Disappearance of the DMSO reflections and emergence of well-defined features at 6.04(2q) and 11.16(2q), 001 and 002
reflections with d values of 14.62 and 7.92 , respectively point out that the DMSO species were substituted efficiently by benzamide
molecules. The thermal stability of the K-Bz derivative up to 300°C can be attributed to the slightly tilted aromatic ring keying into the
gibbsitic sheets via the –NH
2
groups.
Keywords: benzamide, DMSO, inner surface hydroxyls, kaolinite, preadsorption
* Author for correspondence: bafsin@omu.edu.tr