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occupy preferentially the Me2 sites [11]. Single crystal X-
ray diVraction studies of mixed formates CuxMe1¡x
(HCOO)2·2H2O (Me D Mn, x D 0.47; Co, x D 0.35; Ni,
x D 0.37, and Cd, x D 0.47) reveal a clear preference of the
Cu2+ ions to Me1 sites, whereas the Me2+ ions are mainly
localized at the Me2 sites [12].
MgxMn1¡x (HCOO)2·2H2O mixed crystals are reported
and discussed.
2. Experimental
The metal formates, Mg(HCOO)2·2H2O and
Mn(HCOO)2·2H2O, were prepared by neutralization of
dilute formic acid solutions with the corresponding metal
hydroxide carbonate and oxide at 70–80 °C, respectively.
Then the solutions were concentrated and cooled to room
temperature. The mixed magnesium manganese formates
were obtained according to the solubility diagram of the
Mn(HCOO)2¡Mg(HCOO)2¡H2O system at 25 °C [19].
The bulk compositions of the mixed formates were deter-
mined as follows: the sum of the magnesium and manga-
nese concentrations were determined complexometrically
with complexon III at pH 9–9.5 using eriochrome black T
as indicator. Mn2+ ions in the presence of Mg2+ were
determined in the same manner after binding Mg2+ ions
with ammonium Xuoride. The magnesium formate con-
centrations were calculated by diVerence. Samples of
mixed crystals containing matrix-isolated HDO molecules
(isotopically dilute samples, ca. 8–10% D2O) were pre-
pared by the same crystallization procedure in water
partly deuterated. Single crystals were obtained by slow
crystallization from mixed solutions. The reagents used
were “p.a.” quality (Merck).
Single crystal X-ray diVraction data were gathered on a
Bruker AXS SMART APEX CCD diVractometer (radia-
tion: Mo Kꢁ,ꢂ: 0.71069 Å; driving software: SMART [20];
data integration: SAINT [20]; absorption corrections:
SADABS [21]). The main structure was taken from a pre-
vious work on the subject [18], and reWned by least
squares on F2 with anisotropic displacement parameters
for non-H atoms. Hydrogen atoms attached to carbon
were placed at their calculated positions (C–H: 0.93 Å)
and allowed to ride, while those attached to oxygen were
found in the Fourier maps and reWned with no constraints
and free isotropic displacement factors. All relevant calcu-
lations were performed with the computer programs
SHELXS97/SHELXL97 [22] and SHELXTL [23]. Full
use of the CCDC package was also made for searching in
the CSD Database [24]. Crystallographic data (excluding
structure factors) have been deposited with the Cam-
bridge Crystallographic Data Centre as supplementary
publication No. CCDC 628699-6286711. Copies of the
data can be obtained free of charge on application to
CCDC, 12 Union Road, Cambridge CB2 1EZ, UK (fax:
The absorbance infrared spectra were recorded on the
Bruker model IFS 25 Fourier transform interferometer
(resolution <2 cm¡1) at ambient temperature using KBr
discs as matrices. Ion exchange or other reactions with
KBr have not been observed (infrared spectra using Nujol
mulls were also measured). The Lorentz Wtting procedure
was used in order to determine the band frequencies and
intensities.
Recently, a variant of double matrix infrared spectros-
copy has been proposed and applied in order to deduce
the cation distribution in copper containing mixed for-
mates CuxMe1¡x(HCOO)2·2H2O (Me D Mg, Mn, Co, and
Ni) (Cu2+ ions were included in host metal formates in
wide concentration ranges (x 6 0.5) additionally to
matrix-isolated HDO molecules) [13–15,17]. The analysis
of the infrared spectra shows that the regions of the O¡H
vibrations are mostly sensitive to the coordination envi-
ronment of the metal ions present (regions of
3200¡3500 cm¡1 (ꢀOH) and 2300–2500 cm¡1 (ꢀOD of
matrix-isolated HDO molecules)) since the water mole-
cules in the isomorphic formate series exhibit diVerent
hydrogen bond strengths due to both the diVerent
metal¡water interactions (i.e., diVerent synergetic eVect)
and the diVerent unit-cell volumes of the formates (i.e.,
sion of guest ions in host formate matrices will result in
the appearance of new infrared bands for the ꢀOD
modes in the mixed crystals additionally to those due
to the host compounds – Me(g)¡OH2···OCHO¡Me(h),
Me(h)¡OH2···OCHO¡Me(g),
and
Me(g)¡OH2···
OCHO¡Me(g) (g – guest ions; h – host ions; the metal
guest ions are assumed to occupy the two available
positions). The frequencies of the uncoupled ꢀOD modes
for the above hydrogen bond systems depend strongly
on the synergetic eVect of both the guest and the host cat-
ions. If we assume that all Me1 sites are occupied by one
of the ions only, then the Me0.5Me0.5(HCOO)2·2H2O
mixed formate might be considered as a double salt, and
consequently only four bands corresponding to the ꢀOD
modes are expected to appear in its spectrum. The appear-
ance of more than four infrared bands is an indication
that each metal ion is located at the two available
positions.
The water molecules in Mg(HCOO)2·2H2O form the
weakest hydrogen bonds within the isostructural series,
irrespective of the short Mg¡OH2 bond lengths owing to
the ionic character of the respective Mg¡OH2 bonds
[14,17,18]. On the other hand, Mg2+ ions are known to
exhibit a strong aYnity to water molecules. This property
of the Mg2+ ions allows us to assume that when Mg2+ ions
are included in the structure of metal formate dihydrates
they will occupy preferentially the Me2 sites. Our recent
investigations aim at conWrming this assumption. For
example, it has been established in our previous paper [18]
that the Zn2+ ions display a clear preference to Me1 sites,
whereas the Mg2+ ions are localized predominantly at
Me2 ones in MgxZn1¡x(HCOO)2·2H2O mixed crystals.
In the present paper our single crystal X-ray diVraction
and double matrix infrared spectroscopic studies on