Synthesis of Propylene Glycol Monomethyl Ether Over Mg/Al Hydrotalcite Catalyst
97
band of the carbonate anions was observed at 1370 cm-1
(t3) for all the LDHs samples. For the Mg/Al molar ratios
of 0.25, 0.5 and 6.0, this peak split into a double band
indicating a lowering of carbonate anion symmetry and
the disordered nature of the interlayer, which caused the
removal of the degeneracy of the t3 and t4 modes [15]. The
appearance of some very faint absorption at 670–700 cm-1
for the Mg/Al molar ratios of 0.25 and 0.5 implying the
disordered nature, and the band at 687 cm-1 for Mg/Al
molar ratio of 4.0 was strongest in all other samples,
showing that the above interpretation was justified. The
lowering of the symmetry also caused the activation of the
t1 mode around 1050 cm-1, inactive when the carbonate
anion retained its full symmetry [15, 19, 20]. The t1
A
a
b
c
d
e
B
a
b
c
d
e
vibrational mode of carbonate ions appeared at 1060 cm-1
.
The above assumption was supported by the result that the
t1 mode was found for the Mg/Al molar ratios of 0.25, 0.5,
1.0 and 6.0, but not for the Mg/Al molar ratios of 4.0. The
results showed that the LDH Mg/Al 4.0 possessed high
symmetry and ordered nature of the interlayer anions.
The bands around 553 and 770 cm-1 could be assigned to
translation modes of the hydroxyl groups mainly influenced
by the trivalent aluminum but also influenced by probably
Mg2? in its coordination [19]. It could be seen that the
band at 770 cm-1 were clearly observed for all the Mg/Al
molar ratios, and the band at 553 cm-1 for the Mg/Al
molar ratios of 1.0, 4.0 and 6.0, but not for 0.25 and 0.5.
The intensity of the two bands was the highest for the Mg/
Al molar ratios of 4.0. The appearance of absorption band
at around 445 cm-1(d O–M–O) characteristic of lattice
vibrations of [Mg, Al] octahedral sheets demonstrated the
crystallization of the LDHs [21]. The intensity of the sharp
peak at 445 cm-1 increased with decrease in Al concen-
tration in the hydrotalcites with Mg/Al molar ratios of
0.25–4.0, and then decreased in the hydrotalcite with Mg/
Al molar ratios of 6.0. The observed discrepancies among
the LDHs with various Mg/Al molar ratios in FT-IR
spectra were consistent with those in XRD patterns
(Fig. 1). The samples with Mg/Al molar ratios of 1.0 and
4.0 showed pure the hydrotalcite pattern while the others
showed impurities of AlOOH (Mg/Al 0.25 and 0.5) and
MgCO3 (Mg/Al 6.0).
4000 3500 3000 2500 2000 1500 1000 500
Wavenumber (cm-1)
Fig. 2 FT-IR spectra of the LDHs and LDOs samples. A LDHs
samples, B LDOs samples; a Mg/Al 0.25, b Mg/Al 0.5, c Mg/Al 1.0, d
Mg/Al 4.0, e Mg/Al 6.0
3.1.2 FT-IR Spectra
The FT-IR spectra of the Mg–Al hydrotalcites with dif-
ferent Mg/Al molar ratios in the region 400–4000 cm-1
were shown in Fig. 2. For all the hydrotalcites with dif-
ferent Mg/Al molar ratios, the broad band was found at
around 3450 cm-1 (m1-OH-1) and it was ascribable to the
brucite-like layers (OH- stretching vibration), caused by
the interlayer water molecules and hydroxyl groups in the
brucite-like layers [18]. In lower frequency region
(Fig. 2A), a peak at about 1650 cm-1 (d-HOH) in all the
LDHs samples could be attributed to the bending mode of
interlayer water [18, 19]. However, a shoulder around
1650 cm-1, or of a double band in the region 1640–
1660 cm-1, was observed in the cases of Mg/Al molar
ratios of 0.25, 0.5 and 1.0 (B1.0). This might indicate the
presence of a very small amount of aluminum not incor-
porated in the hydrotalcite structure [19]. The carbonate
anion in a symmetric environment was characterized by a
D3h planar symmetry, with three IR active absorption
bands, as well as in the case of the free carbonate anion. In
most hydrotalcites the three bands were observed at 1350–
1380 cm-1 (t3), 850–880 cm-1 (t2) and 670–690 cm-1
(t4) [15]. This was almost what was observed for every
hydrotalcite irrespective of the nature of the octahedral
sheets suggesting full symmetry for the interlayer anions
[20]. The three bands were observed only in the samples
with Mg/Al molar ratios of 1.0 and 4.0, which implied the
Mg/Al molar ratios of 1.0 and 4.0 had a rather symmetric
structure for the interlayer anions. The main absorption
The spectra of the calcined samples (LDOs) were dif-
ferent from those of the precursors (LDHs) (Fig. 2B). The
(m1-OH-1) mode appeared around 3450 cm-1, where
the intensity of the band was obviously lower than that of
the uncalcined samples (LDHs). The weak band at around
1640 cm-1 was observed, but the shoulder in the region
disappeared for the LDO Mg/Al 0.25, 0.5 and 1.0 (B1.0).
The band appeared at around 1390 cm-1 (t3) which was
about 20 cm-1 higher than that of the LDHs, and no
splitting was found for all the LDO samples. The presence
of a band of 678 cm-1 was only in the LDO Mg/Al 4.0 and
123