450
Z.-J. Yang et al. / Catalysis Communications 11 (2010) 447–450
Table 2
Difference of pH value before and after reaction corresponding to the MEG selectivity for different systems.
Carboxylate systems
Selectivity (%)
Phosphate system
Selectivity (%)
Carbonate system
Selectivity (%)
Sulfite system
Selectivity (%)
pH rising
pH rising
pH rising
pH rising
84
92
94
96
96
97
97
98
96
96
97
0.8
0.2
0.2
0.2
0.2
0.2
0.1
0.1
0.1
0.5
0.3
83
85
85
86
88
69
57
64
62
59
54
0.1
0.3
0.1
À0.1
1.0
2.2
4.3
4.6
3.6
2.0
1.6
96
97
97
95
90
–
–
–
–
–
0.2
0.3
0.3
0.3
0.5
–
–
–
–
–
63
67
61
67
–
–
–
–
–
3.2
5.9
6.7
4.8
–
–
–
–
–
–
–
–
–
–
–
with low MEG selectivity dramatically increased after the reaction,
while those with high MEG selectivity only had minor change
throughout the whole reaction process (Table 2). As can be seen,
the pH value increase after the reaction is 2.0 or more for the sulfite
system with low MEG selectivity (<70%), while that for the systems
with high selectivities (>90%), such as carboxylate and carbonate, is
typically 50.5. The same correlation between pH value increase
and MEG selectivity was also observed with the phosphate system
covering a wider range of pH value. It is interesting to note the
sudden transition of pH value as the selectivity decreases from
>85% to <70%. GC–MS results confirmed the formation of glycol
oligomers in solutions encountered pH rising, such as DEG, TEG
and tetraethylene glycol. These by-products containing more ester
linkages can strongly adsorb water and capture H3O+, leading to
the pH of reaction solution alkalization. Once the alkalization hap-
pens, the solution might jump out the pH window to produce more
by-products. And the by-products will further alkalize the solution
through capture H3O+, causing the reaction system to enter a vi-
cious circle and further lower MEG selectivity.
Acknowledgements
This work was supported by NSFC (20721063), STCSM
(075211013 and 08DZ2270500) and Major State Basic Research
Development
Program
of
China
(2009CB623502
and
2009CB623506).
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Several inorganic salt systems were investigated as homoge-
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experimental observations. Two pH windows having pH values of
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