Carbon-13 NMR spectroscopy of sulfonium ylides

Carbon-13 NMR spectroscopy of sulfonium ylides

TetrahedronLettersVol. 21, pp 2109 - 2112 OPergamon press Ltd. 1980.Printedin Great Britain 0040-4039/60/0515-2109#02.00/0 CARBON-13 NHB SPECTROSCOP...

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TetrahedronLettersVol. 21, pp 2109 - 2112 OPergamon press Ltd. 1980.Printedin Great Britain

0040-4039/60/0515-2109#02.00/0

CARBON-13 NHB SPECTROSCOPY OF SULFONIUM YLIDES G.BarbareLla, P.Dembech and A.Garbesi Laboratorio C.N.R.,via Tolara di Sotto,89-OZEANO HMXLIA (Bologna)- ITALY

C-13 NMB data for a series of stabilized and unstabilized ylides indicate flattening at the ylidic carbon with respect to the Parent salts. For unst*ilired ylides association between the oarbanionic center and the lithium cation cannot be neglected. Sulfunium yfides are the intermediates in the B/D base-catafysed exchange' and in the methylation2 of sulfonium safts,both reactions being often highly stereoselective.The results of the exchange reaction have been explained on the basis of a pyramidal ylidic carbon and this interpretation is supported by & lb initio calculations .The results of the methylation reaction may be accounted for either by a planar or by a pyramidal ylidic carbona. Direct experimental evi dence on the structure of sulfonium ylides appears to be a necessary step to e& cidate the factors determining the stereosslectivity of these reactions,in anale gy with what has been done for other sulfur compounds3. To our knowledge only a few proton4 and carbon-13' NMR data on stabilized sulfonium ylides (i.e. bearing electron-withdrawing groups attached to the ylidic carbon) have been reported. On the contrary an abundance of data exists on p~~p~ni~ yli.des,for which ex6,7 perimental and theoretical7 evidence indicates a pyramidal and a planar geomg try at phosphorus and carbon respectively. We present here the C-L3 parameters

( 8,

1

a series of stabifised (l-5) and unstabilized

Sew) of the carbanionic carbon for (6-8) sulfonium ylides,which indi-

cate that the ylidic carbon is more flattened (if not planar) than in the corresponding salts. compounds l-5 are either known compounds or were prepared accord 8 ing to established procedures .Compounds 6-8 were obtained directly in the NMR 9 tube at -70°C by treatment of the salts in THY?-d8 with LiCHC12(1.2 eq.) ,After recording the spectra the starting salts were regenerated by quenching with CH30H:decomposition was less than 20%. Spectra were recorded on a Varian FT-80 spectrometer at probe temperature are in Hz and

(25Lt2W

for l-5 and at -7Wc

for 6-8.

3's

b's are in ppsk with respect to cx32CB or TBP-d 8. The accuracy is 2f09

2112

well

as on the general

aspects

of the geometry

of sulfonium

ylides.

References 1. a)G.Barbarella,P.Dembech,A.Garbesi references

therein;

and A.Fava,J.Am.Chem.Soc

.,1975.5883

and

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..=,8262;

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I

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therein.

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Chem.Soc.,m.353. 8. B.M.Trost p.30-31

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and references

9. E.J.Corey,M.Jautelat 10. a)J.B.Stothers chap.4; 11. T.Durst

Ylides",Academic

Press,New

York,-,

therein. and W.Oppolzer,Tetrahedron

"Carbon-13

Letters,m,2325.

NMR Soectroscony",Academic

Press,New

York,=,

b)u.,chap.9. and M.Molin,Tetrahedron

Letters,1975,63;

tens , ibid .a1978 # 467; G.Chassaing,R.Lett

(Received in UK 10 March 1980)

J.F.Biellmann

and J-J-Vi-

and A.Marguet,ibid.,l978,471.