COMMUNICATIONS
Sudip Mukhopadhyay et al.
produced as a by-product of CH OSO H hydrolysis
could be sent to the Claus process where it would react
Metal Complexes, Kluwer Academic Publishers, Dor-
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3
[
with H S to produce elemental sulfur which would final-
2
ly be transformed to SO by catalytic oxidation with air.
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3
68, 613–615.
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[
1
Experimental Section
[
[
6] J. H. Lunsford, Catal. Today 2000, 63, 165–174.
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Typical Procedure
[
[
8] S. Mukhopadhyay, A. T. Bell, Chem. Commun. 2003,
In a typical reaction, a 100-mL, glass-lined, high-pressure Parr
autoclave reactor was charged with 0.4 mmol of urea-H O ,
1
590–1591.
9] M. Zerella, S. Mukhopadhyay, A. T. Bell, Org. Lett. 2003,
, 3193–3196.
2
2
0
.1 mmol of RhCl , 3.76 g of MSA, and 21 mmol of SO . A
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3
5
small Teflon-coated magnetic stir bar was used to stir the reac-
[
10] G. A. Foulds, B. F. Gray, Fuel Proc. Tech. 1995, 42, 129–
50.
11] J. A. Labinger, J. E. Bercaw, Nature 2002, 417, 507.
12] S. Mukhopadhyay, A. T. Bell, J. Mol. Catal. A: Chem.
tion mixture. The reactor was purged with N to expel the air
2
1
3
and pressurized with 600 psig of CH . The reactor was then
4
[
[
heated to 758C under stirring and kept at that temperature
for 6 h. After the stipulated period of time, the reactor was
cooled, purged with N , and opened to add extra SO to the re-
2
004, 211, 59–65.
2
3
action mixture. The autoclave was then closed, purged with N2
[13] R. A. Periana, D. J. Taube, E. R. Evitt, D. G. Loffer, P. R.
Wentrcek, G. Voss, T. A. Masuda, Science 1993, 259,
340–343.
and then pressurized with 300 psig of N gas and heated slowly
2
o
to 160 C. The reaction mixture was stirred at 1608C for 10 h.
After this period, the reactor was cooled, the pressure was re-
[14] R. A. Periana, D. J. Taube, S. Gamble, H. Taube, T. Sa-
toh, H. Fujii, Science 1998, 280, 560–564.
[15] R. A. Periana, O. Mironov, D. J. Taube, S. Gamble,
Chem. Commun. 2002, 2376–2377.
leased, and the reactor was purged with N gas. The reaction
2
1
13
mixture was analyzed H and C NMR. D O was used in a ca-
pillary as the lock reference. The H NMR chemical shift was
2
1
2.87 ppm to 3.04 ppm for MSA, 3.76 ppm to 3.98 ppm for
[
16] R. A. Periana, G. Bhalla, W. J. Tenn, III, K. J. H. Young,
X. Y. Liu, O. Mironov, C. J. Jones, V. R. Ziatdinov, J.
Mol. Catal. A: Chem. 2004, 220, 7–25.
CH OSO H, 3.13 ppm and 3.83 ppm for CH SO CH , the
3
3
3
3
3
range of chemical shifts in each case depending on the product
1
concentration. A H NMR chemical shift of 3.27 ppm was ob-
[
[
[
[
[
[
17] N. Basickes, T. E. Hogan, A. Sen, J. Am. Chem. Soc.
1
3
served for CH OH. The corresponding C NMR chemical
3
1
996, 118, 13111–13112.
shifts are: 39.5–40.5 ppm for MSA, 60–60.5 ppm for
CH OSO H, and 35.5–36.0 ppm and 58.0–58.5 ppm for
18] M. Asadullah, T. Kitamura, Y. Fujiwara, Angew. Chem.
Int. Ed. 2000, 39, 2475–2478.
19] S. Mukhopadhyay, A. T. Bell, Ind. Eng. Chem. Res. 2002,
3
3
CH SO CH .
3
3
3
4
1, 5901–5905.
20] S. Mukhopadhyay, A. T. Bell, Angew. Chem. Int. Ed.
003, 42, 1019–1021.
21] S. Mukhopadhyay, A. T. Bell, J. Am. Chem. Soc. 2003,
25, 4406–4407.
22] S. Mukhopadhyay, A. T. Bell, Angew. Chem. Int. Ed.
003, 42, 2990–2993.
Acknowledgements
2
This work was supported by a grant from BP as a part of the
Methane Conversion Cooperative.
1
2
[
[
23] R. H. Hass, J. W. Ward, US Patent 4,444,742, 1982.
24] J. Z. Zhang, F. J. Millero, Geochimica Acta 1993, 57,
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