C O MMU N I C A T I O N S
Table 2. Effect of Reaction Conditions on the Sulfonation of Methane to MSAa
CH
psig
4
SO
psig
2
K
mmol
2
S
2
O
8
CaCl
mmol
2
MSA
mmol
% conv. of
CH
psig
4
SO
psig
2
K
mmol
2
S
2
O
8
CaCl
mmol
2
MSA
mmol
% conv. of
entry
T °C
SO
2
to MSA
entry
T °C
SO
2
to MSA
1
2
3
1000
1000
1000
1000
1000
1000
1000
1000
1000
1000
1000
1000
35
35
35
35
35
35
35
35
35
35
35
35
5
5
5
5
5
5
0
1.9
3.7
6.3
5
0
65
65
65
65
65
65
65
65
65
65
45
55
tr
tr.
6
14
22
12
9
0
3
10
7
tr.
13
14
15
1000
1000
200
600
800
1200
1200
1000
1000
1000
1000
35
35
35
35
35
35
0
10
20
25
30
5
5
5
5
5
5
5
5
5
5
5
0.6
0.6
0.6
0.6
0.6
0.6
0.6
0.6
0.6
0.6
0.6
75
85
65
65
65
65
65
65
65
65
65
1.57
1.18
0.92
0.26
0.78
2.1
12
9
7
2
6
16
0
4
9
12
14
0.4
0.6
0.6
0.9
1.8
0.6
0.6
0.6
0.6
0.6
0.6
0.79
1.84
2.89
1.57
1.18
0
0.39
1.314
0.91
tr
c
b
4
16
17
18
19
20
21
22
23
5
6
7
8
9
1
1
1
0
0.53
1.18
1.57
1.84
0
1
2
5
0.79
6
a
Reaction conditions: time, 10 h; solvent, triflic acid, 5 mL. b Time, 26 h. c Time, 72 h.
resulted in a decrease in MSA formation and the detection of a
small amount of methytriflate. The observed decrease in the yield
more than 6.3 mmol of K
2
S
2
O
8
is used can be attributed to the
high rate of formation of O
2
, which can act as a free radical
5
of MSA above an initial K
S O
2 2 8
loading of 5 mmol is possibly
scavenger, thereby inhibiting the formation of MSA. This inter-
pretation is consistent with the failure to observe any MSA when
2
due to the release of O , which, as discussed below, would inhibit
the reaction.
the reaction was carried out with 2-atm O
In conclusion, we have demonstrated a synthetic approach for
the direct, liquid-phase sulfonation of methane with SO . Under
the best reaction conditions, 22% conversion of SO to MSA was
achieved after 26 h of reaction. For this case, 58% of the K
was consumed. Efforts are now in progress to develop a catalytic
process scheme to sulfonate methane with SO in which molecular
is used as the oxygen source instead of K
Acknowledgment. This work was supported by a grant from
2
pressure in the autoclave.
2
The extent of SO conversion observed in 10 h increased with
increasing temperature up to 65 °C. However, a decrease in the
conversion to MSA was observed for temperatures above 65 °C
2
2
(Table 2, entries 11-14).
2 2 8
S O
The conversion of SO
2
to MSA increased from 2 to 14% after
1
6
0 h of reaction when the methane pressure was increased from
00 to 1000 psig, but reached a plateau at 1000 psig. The reaction
2
O
2
2 2 8
S O .
proceeds well even with 200-psig methane pressure. Thus, 7%
conversion of SO to MSA was observed after 72 h (Table 2, entries
5-18).
The reaction rate is also a function of SO
MSA was detected in the absence of SO . This confirms that the
source of SO is neither K nor the solvent triflic acid. At a
SO pressure of 10 psig, only 4% conversion to MSA was achieved.
However, at 25 psig, a 12% conversion was achieved and at 30-
2
Atofina Chemicals, Inc.
1
2
partial pressure. No
References
2
(
1) (a) Hill, C. L. ActiVation and Functionalization of Alkanes; Wiley: New
York, 1989. (b) Axelrod, M. G.; Gaffney, A. M.; Pitchai, R.; Sofranko,
J. A. Natural Gas ConVersion II; Elsevier: Amsterdam, 1994; p 93. (c)
Starr, C.; Searl, M. F.; Alpert, S. Science 1992, 256, 981. (d) Shilov, A.
E. ActiVation of Saturated Hydrocarbons by Transition Metal Complexes;
D. Reidel, Dordrecht, 1984. (e) Olah, G. A.; Molnar, A. Hydrocarbon
Chemistry; Wiley: New York, 1995. (f) Lin, M.; Sen, A. Nature 1994,
368, 613. (g) Sen, A. Acc. Chem. Res. 1998, 31, 550. (h) Labinger, J. A.
Fuel Process. Technol. 1995, 42, 325. (i) Crabtree, R. H. Chem. ReV.
2
2 2 8
S O
2
35 psig, a 14% conversion was obtained (Table 2, entries 19-23).
Solvent composition had a marked influence on the rate of MSA
formation. For the typical reaction conditions, a 2% conversion of
SO to MSA was found as well, using H SO
as the solvent.9
However, in trifluoroacetic acid, 4% conversion of SO to MSA
was attained, and in triflic acid the conversion rose to 14%.
The mechanism of MSA formation from CH and SO is not
1
995, 95, 987. (j) Shilov, A. E.; Shul’pin, G. B. Chem. ReV. 1997, 97,
2
2
4
2879. (k) Dyker, G. Angew. Chem., Int. Ed. 1999, 38, 1698. (l) Gesser,
H. D.; Hunter, N. R. Catal. Today 1998, 42, 183.
2
(
2) (a) Chepaikin, E. G.; Bezruchenko, A. P.; Leshcheva, A. A.; Boyko, G.
N.; Kuzmenkov, I. V.; Grigoryan, E. H.; Shilov, A. E. J. Mol. Catal. A:
Chem. 2001, 169, 89. (b) Periana, R. A.; Taube, D. J.; Evitt, E. R.; Loffer,
D. G.; Wentrcek, P. R.; Voss, G.; Masuda, T. Science 1993, 259, 340. (c)
Periana, R. A.; Taube, D. J.; Gamble, S.; Taube, H.; Satoh, T.; Fujii, H.
Science 1998, 280, 560.
4
2
known; however, it is reasonable to propose that the reaction
involves free radical processes, inasmuch as it was observed that
(
3) (a) Ullmann’s Encyclopedia of Industrial Chemistry; VCH: Weinheim,
O
2
inhibits MSA formation. At least three possible initiators can
be identified, each of which could react with CH to produce CH
radical anions, formed via the
, OH• radicals, produced by the decom-
produced in situ via the reaction of K and
1
994; Vol. A25, pp 503-506. (b) Beringer, F. M.; Falk, R. A. J. Am.
4
3
•
Chem. Soc. 1959, 81, 2997. (c) Young, H. A. J. Am. Chem. Soc. 1937,
59, 811. (d) Murray, R. C. J. Chem. Soc. 1933, 739.
-
•
radicals. These include SO
decomposition of K
position of H
4
(
4) (a) Kroschwitz, J. I.; Howe-Grant, M. Kirk Othmer Encyclopedia of
Chemical Technology; Wiley: New York, 1991. (b) Guertin, R. U.S.
Patent 3,626,004, 1971.
2 2 8
S O
O
2 2
2 2 8
S O
(
(
5) Basickes, N.; Hogan, T. E.; Sen, A. J. Am. Chem. Soc. 1996, 118, 13111.
6) (a) Lobree, L. J.; Bell, A. T. Ind. Eng. Chem. Res. 2001, 40, 736. (b)
Mukhopadhyay, S.; Bell, A. T. Ind. Eng. Chem. Res. 2002, 41, 5901.
the acid solvent, and Cl• radicals, produced via the oxidation of
-
Cl anions. Only OH• and Cl• radicals are thought to play a
significant role in the initiation process, since Table 1 shows that,
(7) Ishii, Y.; Matsunaka, K.; Sakaguchi, S. J. Am. Chem. Soc. 2000, 122,
7390.
in the absence of CaCl
formed. The results presented in Table 1 also suggest that Ca
cations are more effective than other divalent cations in promoting
in situ formation of H and its subsequent decomposition to form
OH• radicals. The CH • radicals once formed could react subse-
quently with SO , K , and methane to form MSA as suggested
2 2
or a mixture of CaO and HCl, no MSA is
(
8) Asadullah, M.; Kitamura, T.; Fujiwara, Y. Angew. Chem., Int. Ed. 2000,
2+
39, 2475.
(
9) In a 100-mL glass-lined Parr autoclave, 5 mmol (1.4 g) K
0.07 g) CaCl , and 5 mL of triflic acid were charged together with a
small Teflon coated magnetic stir bar. The reactor was then purged with
to expel the air out of the system. It was then pressurized first with 35
psig SO (13.14 mmol) and then finally with 1000 psig methane (268
2 2 8
S O , 0.6 mmol
(
2
2 2
O
N
2
3
2
2
2 2 8
S O
mmol) from the adjacent connecting cylinders. The reactor was then heated
to 65 °C under stirring and kept at that temperature for 10 h. After the
stipulated period of time, the reactor was quenched with ice and opened
7
by Ishii and co-workers in the sulfonation of adamantane.
The reason for the observed decrease in the conversion of SO
2
to collect the reaction mixture. The mixture then added slowly to 0.6 g of
1
to MSA when more than 0.9 mmol of CaCl
mixture is not understood. Since the solubility of CaCl
2
is used in the synthesis
in triflic
water and then taken for H NMR analysis. D
2
O and methanol was used
in a capillary as the lock references. The corresponding chemical shifts
for MSA were 2.78-3.02 ppm, depending on the concentration of MSA
in the mixture.
2
acid is limited, a plateau in the conversion level should have been
observed. The observed lowering in the conversion to MSA when
JA0281737
J. AM. CHEM. SOC.
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VOL. 125, NO. 15, 2003 4407