Published on Web 09/26/2002
A Relative Organolithium Stability Scale Derived from
Tin-Lithium Exchange Equilibria. Substituent Effects on the
Stability of r-Oxy- and r-Aminoorganolithium Compounds
Paula Gran˜a, M. Rita Paleo, and F. Javier Sardina*
Contribution from the Departamento de Qu´ımica Orga´nica, Facultad de Qu´ımica, UniVersidad
de Santiago de Compostela, 15782 Santiago de Compostela, Spain
Received January 9, 2002
Abstract: Quantitative thermodynamic stability scales of organolithium compounds can be derived from
measurements of tin-lithium exchange equilibria. A ∆Geq scale of R-oxy- and R-aminoorganolithium
compounds was established, and quantitative stabilization effects of O-alkyl, O-alkoxyalkyl, O-carbamoyl,
N-carbamoyl, and O-carbonyl groups of the R-carbanion are presented. It has been found that an
R-oxycarbanion is far better stabilized by a carbonyl group as the O-substituent than by an alkyl or alkoxyalkyl
group, while the anion-stabilizing effects of the different O-carbonyl substituents are comparable. An
N-carbamoyl group was found to have a somewhat higher stabilizing effect than its O-carbamoyl counterpart.
NMR data are presented that show that benzylic N- or O-substituted carbanions have highly planarized
structures where the negative charge is highly delocalized. The stability data obtained from the tin-lithium
exchanges can be easily converted into “effective pK” data that are useful for predicting the acid-base
behavior of this type of organolithium species.
Introduction
One potential approach to solve this problem could be the
measurement of the pK of the corresponding carbanions,3 since
the basicity of an anion is strongly correlated with its thermo-
dynamic stability, but the determination of the pK of the more
basic, highly functionalized, most synthetically useful carbanions
is still problematic, despite the fact that Streitwieser has provided
data for several types of aromatic, heteroaromatic, and benzylic
systems.4 The measurement of the equilibrium acidities of
hydrocarbon acids under synthetically significant conditions
(approximately 0.1 M ethereal solutions at low temperatures)
is very difficult because proton-transfer equilibration with bases
of known pK (the usual way to determine equilibrium acidities)3-5
take place very slowly in this environment, allowing decom-
position reactions of the involved carbanions to become
competitive.4c An additional inconvenience of the use of acidity
measurements to quantify the stability of organometallic
compounds is that ion pairing and aggregation effects have no
reflection on the pK data, since they refer only to solvent-
separated, nonaggregated species.
R-Heteroatom-substituted organometallic compounds have
gained considerable synthetic status due to their broad utility.
R-Oxy- and R-aminoorganolithium reagents, in particular, have
been the focus of much attention, especially by the groups of
Hoppe and Beak, among others, and a great deal of knowledge
has accumulated about their modes of generation, their con-
figurational stabilities, and the effect of substituents on their
ease of formation and their reactivity,1 but despite all of the
attention devoted to these systems, there remain unanswered
some fundamental questions about this type of reagents. For
instance, it was established very early that both oxygen and
nitrogen atoms considerably increase the stability of an
R-carbanion,1c,2 and yet no data on the quantitative, or even
qualitative, influence of the heteroatom substituents on their
carbanion-stabilizing effects have been reported, despite the
obvious synthetic importance of the results derived from such
a study. This situation is just an instance of a more general,
unresolved problem, that of the development of a method to
quantitatively compare the stability of structurally related,
synthetically useful, highly basic organometallics.
(3) (a) Stratakis, M.; Wang, P. G.; Streitwieser, A. J. Org. Chem. 1996, 61,
3145 and references therein. (b) Bordwell, F. G.; Drucker, G. E.; Fried, H.
E. J. Org. Chem. 1981, 46, 632 and references therein. (c) For an account
of the earlier results see: Cram, D. J. Fundamentals of Carbanion
Chemistry; Academic Press: New York, 1965.
(4) pK of polyhalogenated benzenes: (a) Reference 3a. (b) Streitwieser, A.;
Abu-Hasanyan, F.; Neuhaus, A.; Brown, F. J. Org. Chem. 1996, 61, 3151.
pK of benzylsilanes: (c) Streitwieser, A.; Xie, L.; Wang, P.; Bachrach, S.
M. J. Org. Chem. 1993, 58, 1778. pK of benzyl and fluorenyl hydrocar-
bons: (d) Streitwieser, A.; Ciula, J. C.; Krom, J. A.; Thiele, G. J. Org.
Chem. 1991, 56, 1074. (e) Kaufman, M. J.; Gronert, S.; Streitwieser, A.,
Jr. J. Am. Chem. Soc. 1988, 110, 2829 and references therein.
(5) For other important methods of measuring pK values see: (a) Jaun, B.;
Schwarz, J.; Breslow, R. J. Am. Chem. Soc. 1980, 102, 5741 and references
therein. (b) Arnett, E. M.; Venkatasubramaniam, K. G. Tetrahedron Lett.
1981, 987.
(1) R-Alkoxyorganolithiums: (a) Still, W. C. J. Am. Chem. Soc. 1978, 100,
1481. (b) Still, W. C.; Sreekumar, C. J. Am. Chem. Soc. 1980, 102, 1201.
(c) Sawyer, J. S.; Kucerovy, A.; Macdonald, T. L.; McGarvey, G. J. J.
Am. Chem. Soc. 1988, 110, 842 and references therein. R-Acyloxyorga-
nolithiums: (d) Hoppe, D.; Hense, T. Angew. Chem., Int. Ed. Engl. 1997,
36, 2282 and references therein. (e) Heimbach, D. K.; Fro¨hlich, R.;
Wibbeling, B.; Hoppe, D. Synlett 2000, 950. R-Aminoorganolithiums: (f)
Pippel, D. J.; Weisenburger, G. A.; Faibish, N. C.; Beak, P. J. Am. Chem.
Soc. 2001, 123, 4919. (g) Gross, K. M. B.; Beak, P. J. Am. Chem. Soc.
2001, 123, 315 and references therein. (h) Iula, D. M.; Gawley, R. E. J.
Org. Chem. 2000, 65, 6196 and references therein.
(2) Beak, P.; Zajdel, W. J.; Reitz, D. B. Chem. ReV. 1984, 84, 471.
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10.1021/ja025552r CCC: $22.00 © 2002 American Chemical Society
J. AM. CHEM. SOC. 2002, 124, 12511-12514
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