B.A. Dar et al. / Applied Catalysis A: General 470 (2014) 232–238
233
normal ambient conditions. Therefore, clay supported catalyst as a
substitute of homogeneous catalyst or an expensive heterogeneous
catalyst seems highly desirable [18].
2. Experimental
KSF
2.1. Preparation of the catalyst
Cu/Clay 2b
Cu/Clay 2c
Clay encapsulated Cu(OH)x was prepared by suspending
montmorillonite-KSF (10 g) with cation exchange capacity of 120
meq/100 g clay in 200 ml distilled water and the suspension was
vigorously stirred at 80 ◦C for 2 h. Copper oligomer (base hydrol-
ysed cupric chloride with OH/Cu molar ratio of 2.0) was added drop
wise to acquire the required wt% loading of copper and the result-
ing slurry was stirred at 90 ◦C for 8 h. Heating causes expansion of
clay interlayer and makes the intercalation of Cu-oligomer easy.
The solid products were filtered, washed several times with dis-
tilled water, dried first at room temperature and then at 110 ◦C for
12 h. To study the effect of calcination on the rate of reaction the
catalyst was calcined at different temperatures ranging from 200 to
425 ◦C. The catalyst was characterised by powder X-ray diffraction
using a D-8 ADVANCE (Bruker AXS, Germany) X-ray diffractome-
ter using Ni filter with Cu K␣ radiation Hitachi (H-7500) in the
2ꢀ range 5◦–70◦ in step scan mode (Step size: 0.02◦, Scan speed:
2 s/step). The phases were identified by search match procedure
with the help of DIFFRACPLUS software using JCPDS databank. Tem-
perature programmed reduction (TPR) and BET surface area were
determined by CHEMBET-3000 TPR/TPD/TPO instrument. SEM of
the catalyst was carried out using JEOL.JEM100CXII ELECTRON
MICROSCOPE with ASID Accelerating Voltage 40.0 kV. IR spectra
were recorded on Perkin-Elmer IR spectrophotometer. The spe-
cific surface areas (m2/g) of the catalyst was estimated with the
N2 adsorption and desorption determined at −196 ◦C by means of
an automated CHEMBET-3000 adsorption apparatus. XPS analysis
was performed on a KRATOS-AXIS 165 instrument.
Cu/Clay 2d
5
10 15
20 25 30 35 40 45
50 55 60
2 Theta/ Degree
Cu/clay-2d.
26.7◦, 50.3◦ and 60◦ are due to reflection of the quartz [SiO2]
impurities [19–21] and at 12.5◦, 19.9◦ and 27.9◦ are due to paly-
gorskite [22–24]. Peaks for montmorillonite appear at 2 = 8.9◦ (d
0 0 1 reflection), 19.8◦, 32.2◦, and 62◦ [25,26]. Presence of kaolin-
ite is implied t◦ small peaks at 38.8◦, and 42.5◦ [25,26]. The copper
loaded on montmorillonite-KSF does not show any characteristic
peak of CuO, Cu2O and metallic Cu but peaks with very low intensity
corresponding to mineral atacamite (Cu2Cl(OH)3) and Cu(OH)2 are
observed at 2ꢀ = 16.1, 18◦, 25.1◦, 32.3◦ and 50.3◦ [27–29]. Thus, it
are deposited with very low crystallinity.
The N2 adsorption–desorption isotherm and pore size distri-
bution of Cu(OH)x-clay calcined at 250 ◦C (Cu/clay-2b) are shown
in Fig. 2. The sample displayed type-IV isotherms with H1 hys-
teresis related to capillary condensation steps. Textural properties
such as BET surface area, pore volume (BJH) and the pore radius
(BJH) of Cu(OH)x-clay(Cu/clay-2b) are summarized in Table 1. The
2.2. General experimental procedure for oxidative homocoupling
of arylboronic acid
To a solution of arylboronic acid (1 mmol) in methanol (0.5 ml),
clay encapsulated Cu(OH)x (6 mg) was added and this heteroge-
neous mixture was vigorously stirred at ambient temperature for
30–120 min. After completion of reaction (monitored by TLC), the
reaction mixture was filtered to separate the catalyst. Solvent of
the filtrate was removed under reduced pressure and then worked
up in hexane:water (1:1) system. The aqueous phase was iso-
lated and back extracted with Hexane. The combined organic layer
was dried over MgSO4. The solvent was removed under reduced
pressure and the residue was purified by silica gel column chro-
matography to afford the desired product. The prepared products
were characterized NMR and mass spectral analysis. The spec-
tral data and physical properties thus obtained were compared
with data reported in literature [references herein]. NMR spectra
were recorded on Brucker-Advance DPX FT-NMR 400 MHz instru-
ment. ESI–MS and HRMS spectra were recorded on Agilent 1100
LC and HRMS-6540-UHD machines. Melting points were recorded
on digital melting point apparatus. IR spectra were recorded on
Perkin-Elmer IR spectrophotometer.
3. Results and discussion
3.1. Characterization of the catalyst
The XRD spectra of KSF (montmorillonite-KSF), Cu/clay-2b,
Fig. 2. N2 adsorption–desorption isotherm and pore size distribution curve (inset)
of Cu/clay-2b
Cu/clay-2c and Cu/clay-2d is shown in Fig. 1. Peaks at 2ꢀ = 21◦,