1036
J . Org. Chem. 2002, 67, 1036-1037
Sch em e 1. Su lfon e F or m a tion via th e
Th e F ir st Exa m p le of a Sin glet Oxygen
Hyd r op er oxy Su lfon iu m Ylid e
In d u ced Dou ble Bon d Migr a tion d u r in g
Su lfid e P h otooxid a tion . Exp er im en ta l
Evid en ce for Su lfon e F or m a tion via a
Hyd r op er oxy Su lfon iu m Ylid e
Edward L. Clennan* and David Aebisher
Sch em e 2. P r od u cts fr om P h otooxid a tion of 2
Department of Chemistry, University of Wyoming,
Laramie, Wyoming 82071
Clennane@uwyo.edu
Received October 19, 2001
Abstr a ct: The first example of the formation of a sulfone
concomitant with double bond migration during photooxi-
dation of a sulfide is reported. Evidence is presented which
demonstrates that the double bond migration is not a result
of a prior acid-catalyzed rearrangement of an unrearranged
sulfone precursor. This unusual observation is used to argue
that the sulfone is formed via rearrangement of a hydro-
peroxy sulfonium ylide intermediate.
Sch em e 3
The reactions of singlet oxygen with organic sulfides
have been vigorously studied1-5 since the seminal report
of Schenck and Krauch in 1962.6 The recognition of the
ability of sulfides to act as antioxidants and of their
pivotal role in biological systems has been the driving
force behind the intense interest in these reactions.
Despite the flurry of activity in this area, new fascinating
aspects of these reactions are still being reported. For
example, in 1996 Ishiguro, Hayashi, and Sawaki7suggested
that the small amount of sulfone formation in these
reactions was in part derived from rearrangement of a
hydroperoxy sulfonium ylide, 1 (Scheme 1). Their evi-
dence consisted of the observations that the two oxygen
atoms were derived from the same oxygen molecule and
that isotopic exchange at the R-position accompanied
sulfone formation.
We report here the first example of a double bond
migration during photooxidation at sulfur.8 We also argue
that this reaction provides independent verification of the
role of the hydroperoxy sulfonium ylide, 1, in sulfone
formation.
Photooxidation of a 0.05 M C6D6 oxygen saturated
solution of ethyl γ-phenylthiocrotonate, 2, containing 2.5
× 10-4 M tetraphenylporphyrin to 80% conversion re-
sulted in formation of the products shown in Scheme 2.
Nearly identical results were obtained in CDCl3 with the
exception of the formation of a trace amount of 3SO2 and
formation of 5% of an unknown.
Et3N to provide a thermodynamic mixture of sulfides as
depicted in Scheme 3. These were then treated with 2
equiv of MCPBA to generate the corresponding sulfones
in the same ratio as the sulfide precursors. The structures
of the sulfides and sulfones could be unambiguously as-
signed by examination of the chemical shifts and coupling
constants of the diagnostic HR, Hâ, and Hγ protons.9
The possibility that sulfone 2SO2 could have served
as the precursor of the unanticipated double bond mi-
grated sulfones 4SO2 and 5SO2 was ruled out in two
different experiments. (1) Treatment of the 2SO2:3SO2:
4SO2:5SO2 mixture shown in Scheme 3 with Et3N in
refluxing benzene resulted in the quantitative formation
of 89% of 2SO2 and 11% of 3SO2. The absence of the
double bond migrated isomers 4SO2 and 5SO2 demon-
strate that they are kinetic and not thermodynamic
products in the photooxidation of 2. (2) Cophotooxidation
of methyl allyl sulfide and 2SO2 under the identical
conditions utilized for the reaction of 2 resulted in
Sulfoxide 2SO and sulfone 2SO2 were identical to the
products formed when 2 was treated with 1 and 2 equiv
of MCPBA, respectively. To provide unambiguous as-
signments for the remaining sulfones, 2 was treated with
(8) A double bond migration occurs during the singlet oxygen ene
reaction but in that case the double bond is the seat of reactivity.
(9) 1H NMR (benzene-d6) δ Compound 2 δ 5.75(HR, dt, J ) 16, 1
Hz), ≈ 6.9(Hâ, buried in the aromatic region), 3.00(Hγ dd, J ) 7, 1
Hz); Compound 3 δ 5.60(HR, dt, J ) 11, 1 Hz), 5.87(Hâ, dt, J ) 11, 8
Hz), 4.11(Hγ dd, J ) 8, 1 Hz); Compound 4 δ 2.70(HR, d, J ) 6.5 Hz),
5.96(Hâ, dt, J ) 16, 7 Hz), 6.04(Hγ d, J ) 15 Hz); Compound 5 δ 3.20-
(HR, dd, J ) 7, 2 Hz), 5.95(Hâ, dt, J ) 9, 7 Hz), 6.16(Hγ dt, J ) 9, 2
Hz); Compound 2SO2 δ 5.54(HR, bd, J ) 16 Hz), (Hâ, buried in aromatic
region), 3.20(Hγ dd, J ) 8, 1 Hz); Compound 3SO2 δ 5.61(HR, dt, J )
11, 1 Hz), 5.91(Hâ, dt, J ) 11, 8 Hz), 4.43(Hγ dd, J ) 8, 1 Hz);
Compound 4SO2 δ 2.46(HR, dd, J ) 7, 2 Hz), (Hâ, buried in aromatic
region), 6.00(Hγ dt, J ) 15, 2 Hz); Compound 5SO2 δ 3.67(HR, dd, J )
7, 2 Hz), 6.11(Hâ, dt, J ) 11, 7 Hz), 5.87(Hγ dt, J ) 11, 2 Hz).)
(1) Clennan, E. L. Tetrahedron 2000, 56, 9151-9179.
(2) J ensen, F.; Greer, A.; Clennan, E. L. J . Am. Chem. Soc. 1998,
120, 4439-4449.
(3) Bonesi, S. M.; Albini, A. J . Org. Chem. 2000, 65, 4532-4536.
(4) Bonesi, S. M.; Torriani, R.; Mella, M.; Albini, A. Eur. J . Org.
Chem. 1999, 1723-1728.
(5) Bonesi, S. M.; Mella, M.; d’Alessandro, N.; Aloisi, G. G.; Vanossi,
M.; Albini, A. J . Org. Chem. 1998, 63, 9946-9955.
(6) Schenck, G. O.; Krauch, C. H. Angew. Chem. 1962, 74, 510.
(7) Ishiguro, K.; Hayashi, M.; Sawaki, Y. J . Am. Chem. Soc. 1996,
118, 7265-7271.
10.1021/jo016219t CCC: $22.00 © 2002 American Chemical Society
Published on Web 01/16/2002