3
1
1
3
18
(
P: δ = 20.4; H: δHα = 5.05, δHβ = 3.60, J(H H ) = 5.6,
which has ever been reported for a carbon acid. However, it is
clear that this behaviour is an artefact, being the reflection of
the strong susceptibility of the aldehyde function to covalent
hydration. Interestingly, the available evidence is that the
approach to the 1,H 1 equilibrium is the rate-limiting step of
the overall ionization process. In order to delineate all the
mechanistic facets of the behaviour of this compound, we are
currently focussing our efforts on the design of experimental
conditions allowing a direct kinetic study of this step.
P
α
β
2
3
13
1
J(PH ) = 13, J(PH ) = 4.1; C: δCα = 87.6, δC = 32, J(PC ) =
β
7
α
β
β
1
5
3.3) with no trace at all of the parent aldehyde form. This
makes it reasonable to assume that an essentially complete con-
version of 1 to 1,H occurs at the low substrate concentrations
Ϫ5
Ϫ3
(
≈5 × 10 mol dm ) involved in our kinetic measurements
conducted in the 70%H O–30%Me SO mixture. It follows that
2
2
the ionization of 1 is better depicted by eqn. (3) rather than
CH
+
+
K
a
Ph PCH CH(OH)
Ph PCH CHO
3
2
2
3
2
2 H
H O (K )
β
1
α
,H
1
References and notes
_
1 C. F. Bernasconi, Adv. Phys. Org. Chem., 1992, 27, 119 and refer-
ences therein.
+
ϩ
Ph PCHCHO ϩ H
(3)
3
C-1
2 (a) C. F. Bernasconi and R. L. Montanez, J. Org. Chem., 1997, 62,
8
162; (b) C. F. Bernasconi, J. A. Moreira, L. L. Huang and K. W.
eqn. (1), implying that both the above measured pK and log k0
values are apparent values that we will now refer to as pKa
a
obsd
Kittredge, J. Am. Chem. Soc., 1999, 121, 1674.
3 (a) D. M. Heathcote, J. H. Atherton, G. A. de Boos and M. A. Page,
J. Chem. Soc., Perkin Trans. 2, 1998, 535; (b) ibid., 1998, 541.
obsd
and log k0
.
Based on the above evidence two different arguments can be
4
(a) G. Moutiers, B. El Fahid, R. Goumont, A. P. Chatrousse and
F. Terrier, J. Org. Chem., 1996, 61, 1978; (b) F. Terrier, E. Kizilian,
R. Goumont, N. Faucher and C. Wakselman, J. Am. Chem. Soc.,
1998, 120, 9496.
CH
used to obtain an estimate of the hydration constant K = K
/
H
a
obsd
Ka
. The first is based on previous findings that the relative
acidifying effects of the CHO and CORЈ (RЈ = CH , C H )
groups upon the carbon acidity of compounds of general struc-
ture RCH CORЈ depend very little on the RЈ substituent, e.g.
3
6
5
5 G. Moutiers, A. Peignieux, D. Vichard and F. Terrier, Organo-
metallics, 1998, 63, 1944.
2
COC
6
H
5
CHO
14
CH
6
7
C. F. Bernasconi, Chem. Soc. Rev., 1997, 26, 299.
In accord with previous reports (refs. 8 and 9), C-1 exists as a
mixture of the two cis- and trans-enolate isomers in H O–Me SO
pKa
Ϫ pKa
≈ 3. Based on this difference, a pKa
value of ≈3.50 can be calculated for 1 in 70%H O–30%Me SO.
2
2
obsd
2
2
Combining with pKa
= 5.67 yields K ≈ 150 (pK = Ϫ2.17)
H H
mixtures.
in this solvent. For comparison, a value of K = 37 has been
H
8
9
C. J. Devlin and B. J. Walker, Tetrahedron, 1972, 28, 3501.
N. A. Nesmeyanov, S. T. Berman, P. V. Petrovsky, A. I. Lutsenko
13
reported for the hydration of chloroacetaldehyde.
Providing that the ionization of the aldehyde form remains
the rate-limiting step of the overall process of eqn. (3), another
estimate of K can be obtained from the relationship (4).
and O. A. Reutov, J. Organomet. Chem., 1977, 129, 41.
1
13
31
10 H, C and P NMR spectra show that 2 and 3 exist essentially as
H
the two keto tautomers in H O–Me SO mixtures. See also ref. 9.
2
2
1
1 C. F. Bernasconi, value quoted in ref. 1 (Table 3).
12 X. M. Zhang and F. G. Bordwell, J. Am. Chem. Soc., 1994, 116, 968.
obsd
log k0
= log k ϩ pKH
(4)
0
1
1
3 R. P. Bell, Adv. Phys. Org. Chem., 1966, 4, 1.
4 M. P. Harcourt and R. A. More O’Ferrall, J. Chem. Soc., Perkin
Trans. 2, 1995, 1415.
5 (a) T. J. Burkey and R. C. Fakey, J. Am. Chem. Soc., 1983, 105, 868;
(b) L. H. Funderburk, L. Aldwin and W. P. Jencks, J. Am. Chem.
Soc., 1978, 100, 5444.
Should 1 actually behave as 2 and 3 and exhibit normal
carbon acid behaviour, an intrinsic reactivity typical of a carb-
1
onyl compound should be found with log k ≈ 3–3.5. From eqn.
0
(
4), one thus obtains: pK ≈ Ϫ6.5, a value which combined with
H
obsd CH
pKa
will imply that 1 is a very strong acid (pKa ≈ Ϫ1). In
16 (a) H. J. Cristau and F. Plénat, in The Chemistry of Organo-
phosphorous compounds, ed. F. R. Hartley, J. Wiley and Sons, 1994,
Vol. 3, Chapter 2, p. 45; (b) H. J. Cristau, Chem. Rev., 1994, 94, 1299.
view of the aforementioned relationship governing the carbon
14
acidities of RCH CORЈ (RЈ = H, CH , C H ) compounds,
2
3
6
5
1
13
1
7 δ in ppm relative to Me Si as the internal reference ( H, C) and
4
31
such a conclusion is totally unreasonable. We therefore con-
CH
H PO ( P); J in Hz.
3 4
clude that the set of pK and pK
values obtained in the first
H
a
1
8 F. Terrier, D. Croisat, A. P. Chatrousse, M. J. Pouet, J. C. Hallé and
G. Jacob, J. Org. Chem., 1992, 57, 3684.
approach is more realistic and that the rate limiting step of
eqn. (3) must be the hydration/dehydration pathway and not the
ionization of 1.
In summary, we have found that the ionization of 1 is
formally associated with the lowest Marcus intrinsic reactivity
Communication 9/03667I
1
288
J. Chem. Soc., Perkin Trans. 2, 1999 1287–1288