P. Marakos et al. / Journal of Molecular Structure 650 (2003) 213–221
215
prior to Fourier transformation and zero filled along f1
to 512 points. (c) C–H correlation spectra (HSQC)
were obtained using sensitivity improvement Echo–
Antiecho, phase-sensitive (TPPI) with B0 gradient
pulses for selection of 1H coupled to carbons. A sweep
width of 15 ppm for 1H and 240 ppm for 13C was used
with 128 FIDs in the t1 domain and 1 K data points in
the t2 domain, 48 transients for each t1 increment and
recycling delay 1.5 s. Data were processed using a
shifted sine-square bell and zero filled along f1 to 1024
points. The HMBC experiments were performed
using a low pass J-filter (3.4 ms) and a delay in
order to observe the long-range couplings (65 ms). As
in the HSQC experiments, B0 gradient pulses were
This hydrazide was finally treated with a number of
ketones (acetone, cyclopentanone, cyclohexanone,
cycloheptanone, cyclooctanone, cyclododecanone
and adamantanone) to result in the substituted
hydrazides 1–7.
The assignment of 1H and 13C signals in the NMR
spectra was achieved by the concerted application of
1
COSY, NOESY, HSQC and HMBC experiments. H
and 13C NMR spectra of all compounds in both
solvents show two series of signals.
The 1H NMR data for compounds 1–7 in DMSO-d6
and CDCl3 are provided, for the most relevant protons,
in Table 1 and for the rest Section 4. The alkylidene
protons of the NyCr substituent appear upfield and are
severely overlapped, consequently they are not men-
tioned, except of the deshielded Ha and Hb neighboring
to the imine bond. 13C chemical shifts are summarized
in Table 2 for the most relevant carbons, other
assignments are given in Section 4 (Table S1).
In the 1H spectra in DMSO-d6 solution the chemical
shift difference between the corresponding resonances
in the two series of signals concerning the CH2 and NH
protons are ,0.3 and ,0.1 ppm, respectively.
In the majority of the compounds the two SCH2
protons are almost equivalent and their resonances
exhibit a second order AB system for both series of
signals with the Dn=J ratio ranging from 0.9 to 0.0
(Table 1).
1
applied in order to select H coupled to 13C nuclei,
256 transients with 128 increments in the t1 domain
and 1 K data points in the t2 domain. Data were
processed using a shifted sine-square bell and zero
filled along f1 to 1024 points.
2.4. Molecular calculations
Molecular calculations were performed using
Macromodel 6.5 (Schrondinger) [15] running on
a Silicon Graphics O2 R5000 computer under IRIX
6.3. The MMFF force field was used [16] as
implemented in the Macromodel software. The
Polak–Ribiere (conjugate gradient) minimization
method with an energy convergence criterion of
0.01 kJ/mol was used for geometry optimization.
A 2000 steps conformational search was performed
using MonteCarlo/Low Mode (MC/LMOD) [17]
mixed mode strategy involving systematic search of
low frequency modes (LMOD) or torsional Monte-
Carlo mode (as implemented in the MonteCarlo
Multiple Minimum command in Macromodel/Batch-
min). Volume of the NyCr substituent was calculated
using the VOL mode implemented in Macromodel.
In the phase-sensitive NOESY spectrum cross-
peaks appear, relating the two AB second order
systems of the two different series of signals attributed
to the SCH2 protons (Fig. 2). These cross-peaks exhibit
the same phase as the diagonal peaks characteristic for
a chemical exchange phenomenon. The same type
cross-peaks are observed connecting the two NH
peaks. These signals also present ‘chemical exchange’
cross-peaks with the residual water resonance signal
existing in the DMSO solution.
Moreover, in DMSO-d6 two additional resonances
appear in the spectra at 4.03 and 3.31 ppm when the
samples were prepared in relatively anhydrous
conditions. These signals should originate from
mobile hydrogens as they exhibit chemical exchange
cross-peaks in the EXSY spectrum with the NH and
the residual water peak. They are also shifted together
with the water residual peak when the temperature
increases and vanish when the spectra are recorded in
solutions with more residual water.
3. Results and discussion
For the preparation of the compounds 5-adamantyl-
4-(2,4-dichlorophenyl)-3-mercapto-4H-1,2,4-triazole
[10] reacted with ethyl bromoacetate in alkaline
medium, to give the corresponding mercaptoacetic
acid ethyl ester, which was readily converted to
the hydrazide after treatment with hydrazine hydrate.