Joumal of bfolecultzrStrz~ciuure. 79 (1982) 261-265
FAR INFRARED SPECTRA
OF METAL COMPLEXES
261
in The Netherlands
Ekevier Scientific Publishing Company, Amsterdam -Printed
IN AQUEOUS
SOLUTIONS
C. CARR and P.L. GOGGIN Department
of Inorganic Chemistry,
The University,
Bristol
BS8 1TS (Gt. Britain)
ABSTRACT Using F.t.i.r.
and multiple
acquisition
methods,
good S/N ratios can be obtained from aqueous are presented
for some concentrated
colour precludes separate
cations,
quantitative
bromide
in about 4 hours.
chloride
systems
To obtain spectra without
removal of each component.
halide and gallium(II1)
solutions
ruthenium(II1)
Raman spectroscopy.
water or hydrated
far 1.r. spectra with fairly
subtraction
techniques
Results are presented
where
Spectra the
interference are employed
from for
for some indium( III)
systems.
INTRODUCTION Because of technical i.r. have attracted have reported solutions
of
in examining features results
difficulties,
relatively
and discussed strong
the broad profiles (ref.
aqueous
due to ZnCl vibrations here which demonstrate
readily observed
little attention.
electrolytes
concentrated
studies on aqueous
Dudley Williams
in the far and co-workers
for water (ref. 1) and -1 . Tyler and Querry, down to 75 cm
2)
solutions
observed
of ZnC12 were unable to locate soecific
(ref. 3) in a study-down that metal-halide
from concentrated
solutions
to 300 cm-'.
stretching
(> 1M) aqueous
solutions
features
We report can be
of metal-halide
complexes. METHODOLOGY
AND RESULTS
One difficulty obtaining
ln studying far i-r. spectra
cell windows
with thin films.
which are both transparent
Nicolet 7199A F.t.i.r.
of water
spectrometer
and polyethylene-windowed here are 4 hours
solutions
and sufficiently
Silicon proves to be a suitable material
Fig. 1 shows the spectrum
presented
of aqueous
(12.14 p thickness) Typical
so obtained
acquisition
(1500 scans).
nO22-2860/82/000D-Q000/$02.75@1982Elsevier
rigid for work
for this purpose.
with 6.25 p Mylar beamsplitter,
T.G.S. detector.
has been
Scientifichbli&ingCompany
using a Globar
source
times for examples
a .
b
sbo
430
lbo
‘0
l.lm&&eERs
Fig. 1. Far i.r. spectrum of water (12.14 p in silicon cell). Fig. 2. Far i-r. spectrum of 1.6M RuC13 in water: (A) as measured and (B) after water subtraction. One area where deeply coloured example,
the i-r. method may prove particularly
solutions
concentrated
shown in Fig. 2. water profile;
for which Raman spectroscopy
aqueous
As measured
ruthenium
(B) is obtained
by subtracting
to the formation features shows
the
at 400 cm of
water
spectrum
in
of
8.33M
LiCl
it.
Assuming
systems containing quantitative
4H20
LiCl.
spectrum
GaBr stretching
of
to
quantitatively
(Fig.
3),
where
“free”
water
to remove solvent
example.
Fig. 4
the feature
despite
water,
the is
due
doubtless
the spectrum
lo thickness)
Li+,
on the
less 3H20 per ruthenium,
as in the preceding
pure
on the
1 ower
still rising concentration
subtracted
to
give
which is used for further processing
Fig. 3(B) is the result of carrying water and LiCl respectively;
of
out two separate
the shoulder
at 272 cm
-1
of RuClRu bridging. 2M GaBr3
in
water
does
not
show
since the two broad bands observed
to those found for the other gallium
of 4.6 mol equivalents established
bound
[Li(H20)4]f"
subtractions,
may be indicative
wavenumbers
(12.12
Processing
is much more intense than in
the spectrum of "dissolved
The
complexes.
is
On adding LiCl to RuC13, the
band moves to lower wavenumber
of anionic
etc. IS not as straightforward -1
is superimposed
of the solution
One such
is dark red-brown,
"free".water
that to be the amount of bound water.
intense RuCl stretching
is that of very
is inapplicable.
which
(A) the solute spectrum
basis of the known water concentration assuming
trichloride
valuable
of
LiBr
shows
by Raman spectroscopy
the
formation
(ref. 4).
in CDC13 is shown in Fig. 5 for comparison.
any
features
attributable
below 400 cm"
trihalides. of
[GaBr4]-
The i.r. spectrum
correspond
However,
to
in
addition
(Fig. 5), as also of [~u4~][GaBr4]
263
8 I
_
2ba 3bO l.tfmmd
*JO
btl
r50
‘0
abo
b0
l!iO
abo URVENUMBERS
Fig. 3. Far i.r. spectrum of aqueous RuCl, t 3LiCl (1.7M in Ru): (A) as measured and (B) with water and [Li(H20)4] cation contributions
Fig. 4. Far 1.r. spectrum of 8.33M LiCl in water: (A) as measured and (B) after subtraction of "free" water assuming [Li(H20)4] cation.
subtracted
Silicon
separately.
windowed
cell
(12.12
~1.
187
URVENUtIBERS
solvent
and
(C) spectrum of (CDC13 subtracte
cation
subtraction.
Bu,+N]LGaBr,] in CDC13
Indium iodide with excess NaI shows In contrast
tetrahedral
as the ultimate
[In14]-
[InBr4]- is not formed
ln the aqueous
at Br:In ratios of 4 or more the InBr stretching -1 with no significant contribution around 190 cm ion absorbs.
The substantially
number presumably subtractlon
procedures
whilst this could,
lower wavenumber
due to hydration
(Fig. 6).
InBr3 + LiBr system;
implies a higher coordination
absorption
in part, be due to imperfections a significant
complex
band maximum in the i-r. IS -1 where the tetrahedral at 236 cm
(e.g, [InBrq(H20)2]-).
leave substantial
seems likely that it contains
'0
Fig. 6. Far i.r. spectra of (A) 1.5M “Nal.sInIb.s” in water and (5) [Pentyl,N] [InI,] in CDCIJ . Solvent etc. have been subtracted ln both cases.
FSg. 5. (A) Far i.r. spectrum of 1.5M nLi1.6GaBr4.6" as measured and (B) after
rbo
In this case the
in the 400 cm
-1
region and
in the subtraction
contribution
from hydrated
model
it
indium species.
The
+ Cl- system shows progressive changes with added Cl- (Fig. 7). position reached (InCl stretching maximum at can be reconciled with a hydrated InC14- complex, the currently accepted
In(II1)
We do not believe that the ultimate 255 cm") view
(ref.
5);
reported
that this is close
we note
for solid
[MeSNH] 3[InC16]
2.cm
i!!
(ref.
to
the
i-r.
acti
we stretching
wavenumber
6).
INCL6.S2
Zi%
$’
e w 990
.
I*
b 2bo ibo w%dJnBeRS
kbo
abo
ibo Fig.
b
WFI&JtL
7.
Effect
lb0
Fig. 8. (A) Far i-r. spectrum of 1.7M InI in water (water subtracted) and (8) the result of interactively subtracting the spectrum of [InIb] .
‘0
on far
i.r.
spectra
of
addition of Li Cl to aqueous InCl (Solvent and cation contributionshave been subtracted quantitatively). 3
.
Where several species are present together different
metal:halide
isolating
the
techniques,
spectra
through
conditions of
shown with the spectrum visible,
Fig.
bq
If
simultaneous
of aqueous
the
complexes
of
this
-
arises from a hydrated cationic the
Raman spectrum
frequency, system
ion
the data for
addition
and
A rudimentary There
subtraction
example
is
are two In1 stretches
to [InI,]- as also identified is
interactively
subtracted
from
the result is Fig. 8(B).
This residue
indium iodide complex.
In addition to
has an additional
polarised
by
feature at about the same
as a shoulder on w, of the anion.
We recently published chloride
by multiple
one corresponding
spectrum
should constitute
(Fig. 8).
InI
the spectra under
solution,
equations.
8(A) until it is no longer visible
probably
In-I
of
the higher wavenumber
the Raman spectrum.
or on dilution
individual
a set
in
a preliminary
(ref. 7) where
peaks predominantly
account of measurements
qua1 i tative use of interactive
arising from tetra-,
for the thallium(II1) subtractions
penta- and hexa-chlorothallates
enabled
to be seen.
265 ACKNOWLEDGEMENT We thank
the
S.E.R.C.
for
a grant
to
purchase
the
F.t.i.r.
spectrometer.
REFERENCES 1 2 3 4 5 6 7
D.A. Draegert, N.W.B. Stone, B. Curnette, and D. Williams, J.Opt.Soc.Am., 56 (1966) 64-69. D.A. Draegert and D. Williams, J.Chem.Phys., 48 (1968) 401-407. I.L. Tyler and M.R. Cjuerry, J.Chem.Phys., 68 (1978) 1230-1236. L.A. Woodward and A.A. Nord, J.Chcm.Soc., (1955) 2655-2656. T. Jarv, J.T. Bulmer, and D.E. Irish, J.Phys.Chem., 81 (1977) 649-656. 3. Gislason, M.M. Lloyd, and D.G. Tuck, Inorg.Chem., 10 (1971) 1907-1910. CZZ2C;;;, P.L. Goggin, and M. Sandstrijm, J.Chem.Soc.,Chem.Corun.~ (1981) .