M. Chan-Huot et al. / Journal of Molecular Structure 976 (2010) 282–289
285
2.1.6. N-(pyridoxylidene)-tolylamine hydrochloride (h)
was used as external reference. Some routine NMR spectra of b
to g were measured using a 270 MHz NMR spectrometer.
Pyridoxine HCl (g) (1.6 g, 7.9 mmol, 1 eq) was dissolved in ca.
30 ml of water then oxidized with manganese dioxide (MnO2)
which was freshly prepared from potassium permanganate
(KMnO4, 1.2 g, 7.6 mmol, 1 eq), sodium bisulfite (NaHSO3, 1.6 g,
15 mmol, 10 eq) and 50% sulfuric acid H2SO4 (4 ml) diluted in
60 ml of water. After stirring for 4 h, the solution was diluted by
adding 500 ml of water and p-toluidine (1.2 g, 11 mmol, 1.4 eq)
was added. The pH was adjusted to 7.5 with a 1 N NaHCO3 solution
and left to stir overnight. The Schiff base was filtered and washed
with water then with ether. The product was dried under high vac-
uum. Yield: 1 g (3.5 mmol), 44%, dark yellow powder. Rf = 0.2
3. Results
A
13C NMR titration of 13C2-PLP in H2O (5 mM) was performed
between pH 1 and 12. Typical {1H}13C spectra obtained are de-
picted in Fig. 4. Only the peaks arising from the isotopically en-
riched carbon sites C-40 and C-50 were analyzed, not the small
peaks arising from the carbon sites containing 13C at natural abun-
dance. 1a gives a signal typical for the aldehyde position C-40,
around 194.5 ppm, and a second signal of equal height around
61.0 ppm. The signal of C-40 of 1b is shifted to about 87 ppm be-
cause of the change of the hybridization at this carbon. By contrast,
the chemical shift of C-50 is altered little. At low pH, the hydrate
form dominates and hence the two signals of 1b are larger than
those of 1a, in agreement with previous 15N NMR studies [8]. By
contrast, the signal of 1a dominates above pH 4. The equilibrium
constants for hydration were calculated from the mole fraction ra-
tios, which were derived by signal integration. The results are
assembled in Table 1.
(DCM:MeOH, 10:0.2). IR (KBr):
m = 3115, 2825, 1405, 1005, 815,
495 cmꢁ1 13C {1H} NMR (125 MHz, DMSO-d6): d = 160.7 (d, C-40,
.
3J(13C, 13C) = 2 Hz), 153.2, 148.2, 144.6, 138.2, 137.7, 133.6, 119.9,
114.0, 110.5 (aromatic carbons), 58.9 (t, C-50, 3J(13C, 13C) = 2 Hz),
18.7 (q, CH3).1H NMR (500 MHz, DMSO-d6): d = 9.17 (s, 1H, H-40),
7.98 (s, 1H, H-6), 7.42 and 7.32 (d, H-aromatic of toluidine part),
4.77 (d, 1J(1H, 13C) = 150 Hz, 2H, CH2-OH), 3.33 (s, 3H, CH3). MS
(FAB (+), matrix H2O/glycerol): m/z (%) = 259.4 ([M + H]+, 6),
153.7, 151.8 ([MꢁN–Toluene–H]+, 100), 116.9. MS (FAB (–), matrix
H2O/glycerol): m/z (%) = 257.4 ([MꢁH]ꢁ, 2), 221.8 ([MꢁH–HCl]ꢁ,
2), 152.8 ([MꢁN–Toluene]ꢁ, 100).
½1bꢃ
Kh
¼
ð1Þ
½1aꢃ
13
2.1.7. C-pyridoxal-50-phosphate (1a)
Table 2 collects all 13C chemical shifts measured at the different
A mixture of phosphorus pentoxide (P2O5, 12 g, 84 mmol, 13 eq)
and phosphoric acid (85%, 16 g, 140 mmol, 21 eq) was prepared
and cooled down to room temperature since the mixing evolves
heat. Subsequently, N-(pyridoxylidene)–tolylamine hydrochloride
(h) (1.6 g, 6.6 mmol, 1 eq) was added. The honey-like mixture
was incubated at 45 °C for 7 h. The reaction was quenched with
an aqueous solution of HCl (3.5 ml, 0.1 M) and left overnight. The
crude product was loaded on an ion exchange column (Amberlite
IR 120) and eluted using water as solvent. After lyophilizing, PLP
was obtained as a yellow solid. Yield: 470 mg, 24%, yellow solid.
pH values. Generally, average chemical shifts of species subject to
different protonation states can be expressed as a function of pH
using the Henderson–Hasselbalch equation [11] adapted for NMR
spectroscopic methods in the fast proton exchange regime [12].
For PLP, which has five protonation states 0 to IV according to
Fig. 1, this equation can be written in the following form [8].
10pH—pK
ai
X
dobs ¼ d0 þ
ðdiþ1 ꢁ diÞ
;
i ¼ 0 to IV
ð2Þ
1 þ 10pH—pK
ai
i
IR (KBr):
m .
= 3365, 2925, 1630 cmꢁ1 13C {1H} NMR (125 MHz,
As usual, pKai represents the pH values where protonation
states i and i + 1 are at the same concentration. di represents the
limiting chemical shift of protonation state i. Eq. (2) is valid for
all nuclei of PLP.
D2O): d = 195.6 (C-40, 3J(13C, 13C) not observable, aldehyde form),
163.6 (d, C-6), 151.3 (s, C-5), 135.4 (s, C-4), 125.5 (s, C-2), 123.6
(s, C-3), 89.4 (d, C-40, 3J(13C, 13C) not observable, acetal form),
61.7 (t, C-30), 15.6 (q, C-20). 1H NMR (500 MHz, D2O): d = 10.4 (d,
The 13C chemical shifts of the aldehyde form 1a and of the hy-
drated form 1b of PLP in Table 2 are plotted in Fig. 5 as a function of
pH. The solid lines were calculated using Eq. (2), optimizing the pKa
values and the limiting 13C chemical shifts. The results are given in
Tables 3 and 4.
13
1J(1H, C) = 185 Hz, 1H, H-40 – aldehyde form), 8.1 (s, 1H, H-6 –
aldehyde form), 6.4 (d, 1J(1H, C) = 170 Hz, 1H, H-40 – hydrate
13
form), 5.2 (dd, 1J(1H, 13C) = 150 Hz, 2J(1H, H) = 5 Hz, 2H, H-30 –
1
aldehyde form), 5.1 (dd, 1J(1H, 13C) = 150 Hz, 2J(1H, 1H) = 5 Hz, 2H,
H-30 – hydrate form), 2.6 (s, 3H, H-20 – aldehyde form), 2.5 (s,
3H, H-20 – hydrate form).
4. Discussion
2.2. Sample preparation
In the first part of this section, we discuss the pH-dependent
equilibrium between the aldehyde form 1a and the hydrate form
1b. In the second part, we discuss the different protonation states
observed here, and compare these results with those obtained pre-
viously [8] using 15N NMR of PLP labeled with 15N in the pyridine
ring.
Aqueous solutions of PLP (5 mM) were prepared using water or
heavy water degassed and stored under argon in order to remove
oxygen and carbon dioxide. The pH values of the solutions were
adjusted before each spectroscopic measurement by addition of
degassed 3 M, 1 M or 0.1 M sodium hydroxide or hydrochloric acid
solutions. For that purpose we used a HANNA HI 9025 pH meter
equipped with a HAMILTON Spintrode P electrode. The pH values
were measured after the experiments and showed an average error
of 0.15.
4.1. Equilibrium between aldehyde and hydrate form
In Fig. 6, the mole fractions of the aldehyde form 1a and of the
hydrated form 1b are plotted as a function of pH. Qualitatively, it
has been known for a long time that 1b dominates at low pH
and 1a at high pH. However, the 13C experiments here allowed
us to elucidate the pH of 4.2 where the equilibrium constant of
hydration Kh is unity.
2.3. Spectroscopic methods
NMR spectra of pyridoxal-50-phosphate were measured using a
Bruker AMX 500 spectrometer (500.13 MHz for 1H, 125 MHz for
13C) at 278 K. The 13C spectra were recorded in the inverse gated
1H-decoupled mode using H2O as solvent, with field locking using
a D2O containing capillary. The recycle delay was set to 10 s. TMS
A consequence of the hydration equilibrium is that it is difficult
13
to determine the C chemical shifts of C-501a at low and of 1b at
high pH.