A R T I C L E S
Perrin and Dong
lone pair. The first H on a methyl will thus take this position
and lead to an increase in acidity of a CHD2NH+ over CD3NH+.
An additional H, as in a CH2D, cannot take that position, so
that the increase in acidity will be less, and also less for CH3.
Thus, the IE per H will decrease as the number of H increases,
or the IE per D will increase as the number of D increases.
This is the direction of the nonadditivity that we have predicted
and endeavored to test.
no lag of one chemical shift behind the other. As a result, minute
imbalances of acidities are detectable. Moreover, because the
titration is performed on a mixture of the two acids, under
conditions guaranteed identical for both, it avoids systematic
errors due to impurities that arise in the synthesis of one of the
isotopologues but not the other. It has recently permitted
measurement of secondary deuterium IEs in carboxylic acids
and phenols.18
Success for this study can be anticipated from the preference
for equatorial deuteriums in 1,3,5,5-tetramethylhexahydropyri-
midine-2-d and 1-methylpiperidine-cis-2,6-d2,12 and from the
elegant demonstration of diastereotopic H in 1,2-dimethylpip-
eridine-1-d, owing to perturbation of the rotameric equilibrium
of the NCH2D fragment.13 Those are cases of isotopic perturba-
tion of a conformational equilibrium, whereas this study involves
a chemical reaction, with N-H bond-breaking or bond-making,
and where the conformational equilibrium affects only one side
of the equilibrium.
The titration can be performed on either the amine or the
ammonium ion. We chose to titrate the amine hydrochloride
with an anionic base, which has the advantage of maintaining
constant ionic strength and reducing medium effects on chemical
shifts. For solvents we chose DMSO-d6, with KOtBu as base,
and D2O, with NaOD as base. The IE on the basicity of
(CH3)2NH had been found to be smaller in D2O,1 owing to
hydrogen bonding to the lone pair, which reduces the n-σ*
delocalization that is responsible for the IE.1,2,12 Consequently,
DMSO offers the better prospect for detecting the nonadditivity,
but it is also subject to random variations in its water content.
Therefore, we measured IEs in both DMSO and D2O.
The key comparison is between the IE on the basicity of
(CH2D)3N relative to (CH3)3N and that on (CHD2)3N relative
to (CH2D)3N, each of these due to three additional deuteriums.
To confirm these values, the composite of these two IEs can be
measured from the comparison of (CHD2)3N with (CH3)3N, due
to six additional deuteriums. To be comprehensive, it is also
possible to measure the IE of eight deuteriums by comparing
trimethylamine with trimethylamine-d8. All of these isotopo-
logues are readily synthesized by standard procedures. We now
report not only that deuteration decreases the acidity constant
Ka of trimethylammonium ion (as had been known) but also
that the IE is nonadditive, in that the decrease, per deuterium,
increases with the number of deuteriums.
Nonadditivity is a powerful test for whether this IE might be
of inductive origin. Although protium cannot simply be more
electron-donating than deuterium,14 an alternative is an elec-
trostatic interaction between the N+ and the dipole moment of
the C-H bond, which is longer than C-D, owing to anharmo-
nicity.15 The dipole moments involved are exceedingly small,
though. Besides, the interpretation in terms of ZPEs is consistent
with the observation that the isotopomer of 1-benzyl-4-meth-
ylpiperidine-2,2,6-d3 with deuterium trans to the methyl group
is more basic.1 Nevertheless, an inductive effect ought to be
linear in the number of deuteriums, and nonadditivity would
be strong evidence against an inductive origin for these IEs.
An NMR titration method makes it possible to measure IEs
on basicities or acidities with great precision. The method
depends on isotope shifts,16 which lead to separate, resolvable,
and assignable signals for isotopologues. The procedure involves
successive additions of small aliquots of base to a mixture of
acids. The stronger acid will be deprotonated first. Its chemical
shift will then move ahead of that of the less acidic one, which
lags behind. The acidity constants Ka and chemical shifts δ of
both H and D acids can be related through eq 1,17 where δ+ or
δ0 is for the ammonium ion or amine, respectively, as measured
at the beginning or end of the titration. Therefore, a plot of the
quantity on the left vs (δH - δH0)(δD+ - δD) should be linear,
Experimental Section
1
NMR Spectroscopy. H and 13C NMR spectra were recorded
on a Varian Mercury 400 or Unity 500 spectrometer. All deuterium
decoupling experiments were recorded on a Varian Mercury 400
spectrometer with a decoupling frequency calibrated from a 2H
NMR spectrum for amine C-D (not D2O or DMSO-d6). After each
1
aliquot was added, the field homogeneity was shimmed on a H
NMR spectrum with deuterium lock, and then the cables were
switched and a 1H NMR spectrum was recorded with WALTZ
decoupling through the lock channel. The spectral window was
reduced to 700 Hz for 1H NMR at 500 MHz or to 600 Hz for
deuterium decoupling at 400 MHz, and the data were zero-filled
to increase digital resolution. Proton chemical shifts in aqueous
solutions are relative to acetonitrile (δ 2.05) as the internal standard,
or to cyclohexane (δ 1.42) in DMSO-d6. All chemical shifts were
read as Hz, to avoid roundoff error in conversion to ppm. To help
distinguish the peaks, an initial spectrum of a mixture of deuterated
species and internal standard was obtained, and then the undeu-
terated or another deuterated compound was added.
Synthesis. After several unsuccessful attempts by various
procedures that gave intolerably large contamination by
CH3(CH2D)2N, tri(methyl-d)amine hydrochloride [(CH2D)3N·HCl]
was obtained by reaction of tris(chloromethy1)amine19 with NaBD4.
This procedure was adapted from the reaction with sodium
methoxide in methanol,20 but in D2O to guard against H incorpora-
tion. Indeed, CH3(CH2D)2N did appear when D2O was replaced
by methanol or H2O. The successful synthesis is remarkable in view
of the extreme hygroscopicity and expected hydrolytic reactivity
h
d
with zero intercept. The ratio of acidity constants, Ka /Ka , can
then be evaluated as the least-squares slope of that plot.
0
0
(δH+ - δH)(δD - δD ) ) (Kah⁄Kad)(δH - δH )(δD+ - δD)
(1)
This method is capable of exquisite precision, because it is
based only on chemical-shift measurements. It does not require
accurate control of pH or volume or molarity or equivalents of
base added, as is usual in pH titrations. The method is
comparative. If there is no difference in acidities, there can be
(12) Anet, F. A. L.; Kopelevich, M. Chem Commun. 1987, 595. Forsyth,
D. A.; Hanley, J. A. J. Am. Chem. Soc. 1987, 109, 7930.
(13) Anet, F. A. L.; Kopelevich, M. J. Am. Chem. Soc. 1989, 111, 3429.
(14) Weston, R. E., Jr. Tetrahedron 1959, 6, 31.
(15) Halevi, E. A. Prog. Phys. Org. Chem. 1963, 1, 109.
(16) Batiz-Hernandez, H.; Bernheim, R. A. Prog. Nucl. Magn. Reson.
Spectrosc. 1967, 3, 63. Jameson, C. J.; Osten, H. J. Annu. Rep.
NMR Spectrosc. 1986, 17, 1. Hansen, P. E. Prog. Nucl. Magn. Reson.
Spectrosc. 1988, 20, 207. Dziembowska, T.; Hansen, P. E.; Rozwa-
dowski, Z. Prog. Nucl. Magn. Reson. Spectrosc. 2004, 45, 1.
(17) Perrin, C. L.; Fabian, M. A.; Armstrong, K. B. J. Org. Chem. 1994,
59, 5246. Perrin, C. L.; Fabian, M. A. Anal. Chem. 1996, 68, 2127.
(18) Perrin, C. L.; Dong, Y. J. Am. Chem. Soc. 2007, 129, 4490.
(19) Fluck, E.; Meiser, P. Angew. Chem., Int. Ed. Engl. 1971, 10, 653.
(20) Fluck, E.; Meiser, P. Chem. Ber. 1973, 106, 69.
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11144 J. AM. CHEM. SOC. VOL. 130, NO. 33, 2008