´
242
A. Gojmerac Ivšic et al. / Journal of Molecular Structure 990 (2011) 237–243
(a)
(b)
-3
c
(HZ)=2x10-3 mol dm
0.9
0.7
0.5
0.3
0.1
-
4
c
(Fe(III))=1.3x10 mol dm-3
0.7
0.5
0.3
0.1
-3
c
(HZ)=5x10-4 mol dm
-
4
c(Fe(III))=1x10 mol dm-3
-3
c
(HZ)=2x10-4 mol dm
400 500
3.0 4.0 5.0 6.0 7.0 8.0 9.0
600
pH
Wavelength / nm
Fig. 9. (a) Dependence of the absorbance of extracted Fe(III)–HZ complex on pH in the aqueous phase. c(HZ) = 1 ꢂ 10ꢀ3 mol dmꢀ3; (b) absorption spectrum of extracted
Fe(III)–HZ complex in chloroform at various HZ concentrations. c(Fe(III)) = 1 ꢂ 10ꢀ4 mol dmꢀ3
.
complexes are shown in Fig. 6a. In the pH range between ꢄ6.5 and
ꢄ5.2 the spectra exhibited bathochromic and hypochromic shifts,
accompanied by the occurrence of a well defined isosbestic point
at 488 nm. That clearly indicated the existence of an equilibrium
between two spectrally distinct species. Another isosbestic point
appeared at 520 nm in the 5.3–3.1 pH range. Below pH = 3.1 fur-
ther decrease of absorbance and bathochromic shift were ob-
served. It should be noted that above pH ꢄ 7 a slight and slow
precipitation (presumably of the uncharged ferric tris(HZ) com-
plex) occurred which made spectrophotometric observations unre-
liable. The spectral data were analyzed by the pHab program.
Among several chemically reasonable speciations used, the best
fit (Fig. 6b) was obtained by assuming the presence of the follow-
phase. The results showed that pH about 6 is optimal for the
extraction of iron(III) with HZ into chloroform (Fig. 9a). The com-
plex species extracted from the aqueous solution was presumably
the uncharged ferric tris(HZ) complex. The absorption spectra of
Fe(III)–HZ complex extracted in chloroform with various HZ con-
centrations are shown in Fig. 9b. The extraction efficiency at opti-
mal pH for the extraction of iron(III) was found to be about 95%.
4. Conclusion
A new 4-pyridone derivative was prepared and explored as
iron(III) complexing agent. Its X-ray crystal structure was deter-
mined as an ethyl acetate solvate.
ing species in the reaction mixtures FeHZ3+, FeHZ22þ, FeH2Z3þ and
2
The values of protonation constants of free HZ were determined
in aqueous solution (Ic = 0.1 mol dmꢀ3 (NaCl), t = 25 °C). The com-
plexation of iron(III) by this ligand was investigated at different
pH values and various Fe(III):HZ molar ratios. Global stability con-
stants of ferric mono-, bis- and tris(HZ) complexes in aqueous solu-
tion (Ic = 0.1 mol dmꢀ3 (NaCl), t = 25 °C) were determined by
means of the spectrophotometric–potentiometric titration.
The extraction of Fe(III)–HZ complexes from aqueous to organic
phase was preliminary studied. The pH of aqueous phase optimal
for extraction was assessed to be about 6, and the extraction effi-
ciency for iron(III) at this pH was found to be about 95%.
FeZ3 (Z denotes fully deprotonated HZ). The calculated global sta-
bility constants of these complexes are listed in Table 4, and their
charge-transfer absorption spectra are shown in Fig. 7.
In the ferric mono(HZ) complex (FeHZ3+) the proton is most
likely bound to the amino group of the ligand. The same holds
for the ferric bis(HZ) complexes FeHZ22þ and FeH2Z3þ, whereas
2
the coordinated ligands in the FeZ3 complex are fully deproto-
nated. Distribution of the complex species as a function of pH is
given in Fig. 8, and is qualitatively in agreement with the results
obtained by Job’s method (Fig. 5).
3.4.2. Studies of the extraction
Supplementary material
The distribution of HZ between chloroform and aqueous
solutions of different acidity and ionic strength was studied. The
concentration of HZ in the aqueous phase was measured spectro-
photometrically using standard concentration–absorbance curves
established previously. These measurements were made at
288 nm. In the concentration range used the solutions of HZ
obeyed Beer’s law. The aqueous media were saturated with chloro-
form and then equilibrated with an equal volume of solutions of HZ
in chloroform for 1 h. Three different concentrations of HZ were
used and the same results were obtained if the initial concentra-
tion in chloroform was 5 ꢂ 10ꢀ5, 1 ꢂ 10ꢀ4 or 1 ꢂ 10ꢀ3 mol dmꢀ3
(Table 5). The distribution coefficient (D) was also independent
of the mineral acid used in the aqueous phase as well as of the ionic
strength. However, distribution of HZ depended on the acidity of
aqueous phase. The increase of acidity resulted in lower distribu-
tion coefficient (Table 5) due to the formation of protonated
cationic species which were better solvated with water in
comparison to chloroform.
Supplementary crystallographic data sets for the structure of
HZꢁEtOAc are available through the Cambridge Structural Data
base with deposition number 771960. Copies of this information
may be obtained free of charge from the director, CCDC, 12 Union
Road, Cambridge CB2 1EZ, UK (fax: +44 1223 336 033; e-mail:
Acknowledgements
We wish to thank the Ministry of Science, Education and Sports
of the Republic of Croatia for the support of this work (Projects
119-1191344-3121, 119-1191342-2959, 119-1193079-1084, 119-
1191342-2960).
References
ˇ ´
[1] K. Jakopcic, B. Tamhina, F. Zorko, M.J. Herak, J. Inorg. Nucl. Chem. 39 (1977)
1201.
[2] M. Tsuchiya, K. Kohata, T. Odashima, H. Ishii, Anal. Sci. 11 (1995) 343.
[3] M.A. Santos, M. Gil, S. Marques, L. Gano, G. Cantinho, S. Chaves, J. Inorg.
Biochem. 92 (2002) 43.
3.4.3. The extraction of iron(III) into the organic phase
Preliminary investigations were carried out to explore the pos-
sibility of the extraction of Fe(III)–HZ complexes into the organic
[4] R.A. Yokel, Coord. Chem. Rev. 228 (2002) 97.