A R T I C L E S
Perrin and Karri
1
1
4.0 M DCl/D
2
O were added and 13C NMR spectra were recorded
3
31 K, corresponding to a ∆pK
a
of 0.09. This agrees well
with the second value in aqueous solution and also with the IE
derived from vibrational frequencies calculated at the B3LYP/
after each addition, until there was no further change in chemical
shifts. The number of aliquots varied from 12 to 20. For each
deuterated pyridine isotopologue at least two carbons undergo
substantial changes in chemical shifts upon N-protonation and were
thus suitable as reporter nuclei. When necessary, signals of the
isotopologues were assigned from the stoichiometry or by adding
authentic undeuterated material. For carbons attached to D the
chemical shift of the central component of the CD triplet or of the
cc-pVTZ level. However, the agreement with the solution ∆pK
a
may be fortuitous.
We therefore have undertaken to resolve the disagreement
between the two measurements in aqueous solution. This topic
is of further interest because of the recent discovery of a low-
temperature polymorph of pyridine-d
5
, different from that of
Also, all the previous IE studies addressed only
, and the errors of (0.02 precluded measurement of
3
CD septet was used.
1
2
Instrumentation. All H NMR spectra and all 13C NMR spectra
1
pyridine-h
pyridine-d
5
.
of lutidine were recorded on a JEOL ECA500 spectrometer. All
5
1
3
the small contributions of individual deuteriums. It would be
informative to distinguish the separate contributions from the
various positions around the ring as well as to assess the IE of
C NMR spectra of pyridines were recorded on a Varian VX-500
spectrometer (125 MHz), using an XSense direct-detection cold
probe. A 7.0-µs, 45° excitation pulse, 128-800 acquisitions, 32K
data points zero-filled to 128 K, and standard broad-band 1
H
3
CD groups in 2,6-lutidine (2,6-dimethylpyridine).
decoupling were used, with the temperature regulated at 298 K.
Data Analysis. Chemical shifts at various pyridine positions
during the course of a titration of a pair of isotopologues were
NMR titration can measure relative basicities with great
1
3
precision. When successive small aliquots of acid are added
to a mixture of bases, the one that is more basic is preferentially
protonated. Its chemical shift thus moves ahead of that of the
H
D
analyzed according to eq 1. The resulting values of K
a
/K
a
were
H
D
converted to ∆pK () log10(K /K )) and averaged for each
a a
less basic one. The acidity constants K
a
and chemical shifts δ
isotopologue. Because precision varied with the reporter nucleus,
weighted averages were calculated (weighted inversely to the square
of the standard deviation), and associated errors are either errors
of the weighted average or standard errors of the mean, whichever
is larger.
0
+
can then be related through eq 1, where δ or δ is the shift for
the deprotonated or protonated form, respectively, as measured
at the beginning or end of the titration. Therefore a plot of the
0
+
quantity on the left vs (δ
H
- δ
H
)(δ
D
D
- δ ) should be linear
Computations. Ab initio density-functional calculations on
with a zero intercept and with a slope equal to the ratio of acidity
constants. Any reporter nucleus can be utilized for this purpose,
pyridine, pyridinium ion, and their 2,6-dimethyl derivatives were
16
performed at the B3LYP/cc-pVTZ level, as recommended, using
1
3
but C is most suitable because its chemical shifts are quite
sensitive to the state of pyridine protonation and because there
are several nuclei in the molecule that provide independent
17
Gaussian 03, Revision D.01. Harmonic vibrational frequencies
0 2 2 5 3 2 2 2
for d , 2,6-d , 3,5-d , 4-d, d , (CD ) , and anti-(CH D) isotopologues
were calculated at very tightly optimized geometries on an ultrafine
optimization grid. The contributions from molecular masses and
moments of inertia, or from the product of vibrational frequencies
H
D
a a
measurements of K /K .
1
8
+
H
0
D
H
a
D
a
0
H
+
D
via the Redlich-Teller product rule, are negligible and are
ignored. The double difference, ∆∆Σν, of sums of all the frequen-
cies of the four species was calculated according to eq 2. This
difference was then converted through zero-point energies to a
calculated ∆pK at 298 K. A separate ∆∆Σν for high-frequency
(
δ - δ )(δ - δ ) ) (K /K )(δ - δ )(δ - δ )
H
D
H
D
(
1)
We now report highly accurate position-specific secondary
deuterium IEs on the basicities of pyridine and 2,6-lutidine. We
have also modeled the IEs by ab initio computations. In all cases
deuterium substitution increases basicity, and we attribute the
IEs to changes of vibrational frequencies on N-protonation.
-
1
C-H vs C-D stretching modes (frequencies > 3000 cm or 2100
-1
cm , respectively) could also be obtained. For the pyridine
isotopologues vibrations can be distinguished as in-plane and out-
of-plane, according to the z components of the displacements, and
a ∆∆Σν due to all the in-plane vibrations was extracted.
Experimental Section
∆
∆ΣV ) (ΣVHPy
+
- ΣVHPydn+) - (ΣVPy - ΣVPydn
)
(2)
Preparation of Deuteropyridines. Except for commercially
5
available pyridine-d , each deuteropyridine or dideuteropyridine was
prepared from the corresponding bromopyridine or dibromopyridine
Results
1
4
with two portions of excess Zn dust in D
Lutidine-2,6-(CD was prepared by two successive exchanges in
O containing K
2 4 2
SO /D O at 90 °C. 2,6-
)
2
The intrinsic isotope shift due to deuteration is always to
lower frequency (upfield), except for C3,5 of lutidine-2,6-(CD ) .
3
1
5
D
2
2 3
CO at 180 °C, but in a Biotage Initiator
microwave oven at 15 bar. Incorporation of deuterium to >95%
3
2
13
C NMR chemical shifts of pyridines and pyridine isotopo-
1
was verified by H NMR.
logues at the beginning and end of titration are listed in Table
S1. Experimental data from NMR titrations of deuterated
pyridine isotopologues are listed in Table 1. For every titration
the correlation coefficient R for the linear fit to eq 1 was greater
than 0.99995, except for C4 of 2,6-lutidine, where R drops to
Preparation and Titration of NMR Samples. Pyridine samples
(
∼1:1 H/D) were prepared as 1.0 M solutions in D
dimethoxybenzene as the internal standard (δ 114.5) and with a
small aliquot of NaOD/D O to guarantee that the pyridine was fully
deprotonated. The 2,6-lutidine sample was prepared similarly, but
in 20% DMSO-d in D O, owing to a lower solubility. The samples
were then degassed under vacuum. Successive 5-µL aliquots of
2
O with 1,4-
2
0
.9998 because the intrinsic isotope shift of the distant deute-
6
2
riums is insufficient to resolve the isotopologues near the
beginning and end of the titration. Figure 1 shows not a typical
plot, but the second worst such plot, for C2,6 of pyridine-d
for which the slope is 1.0828 ( 0.0030 but for which R is only
.99995.
5
,
(
(
11) Mu n˜ oz-Caro, C.; Ni n˜ o, A.; D a´ valos, J. Z.; Quintanilla, E.; Abboud,
J. L. J. Phys. Chem. A 2003, 107, 6160.
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S.; Yamamuro, O. Angew. Chem., Int. Ed. 2009, 48, 755.
0
(
13) Perrin, C. L.; Fabian, M. A.; Armstrong, K. B. J. Org. Chem. 1994,
(16) Szafran, M.; Koput, J. J. Mol. Struct. 2001, 565-566, 439–448.
(17) Frisch, M. J.; et. al. Gaussian 03, revision D.01; Gaussian, Inc.:
Wallingford, CT, 2004.
5
9, 5246. Perrin, C. L.; Fabian, M. A. Anal. Chem. 1996, 68, 2127.
(
(
14) Huber, S.; Grassi, G.; Bauder, A. Mol. Phys. 2005, 103, 1395.
15) Kebede, N.; Pavlik, J. W. J. Heterocycl. Chem. 1997, 34, 685.
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1
2146 J. AM. CHEM. SOC. 9 VOL. 132, NO. 34, 2010