Figuerola et al.
pairwise interactions are antiferromagnetic, there is the
possibility of spin frustration if the three pairwise interactions
are the same; then, only two of the three spin constraints
can be satisfied simultaneously, and the system is geo-
metrically frustrated. The ground state then is of intermediate
spin, intermediate between the lowest and the highest spins
possible for the three metal ions. It is well-established that
the µ3-oxo bridge in [M3O(O2CR)6L3]n+ complexes is
dominant in propagating the exchange interaction.1b,c Oxo-
centered trinuclear complexes of antiferromagnetic spins are
quite common for transition metal ions like Fe3+,2 Mn3+,1c,3
and Cr3+.2k,4 The isotropic Hamiltonian for the interaction
between any two spins can be written as the scalar product
of the spin operators: H ) -ΣijJijSiSj. Therefore, the energy
is minimized for collinear parallel or antiparallel spin
alignments. The available experimental data are in good
agreement with the isotropic HDVV model in the region of
relatively high temperatures. However, there are a number
of serious discrepancies between the predictions of the theory
and the experimental data at low temperatures. In order to
interpret the magnetic properties of these frustrated systems,
it is necessary to go beyond the framework of the above
isotropic exchange model and to introduce an antisymmetric
exchange interaction, GAB. This antisymmetric exchange
interaction of the type
HAS ) ΣijGij[Si × Sj]
where Gij ) -Gij is the antisymmetric vector constant. As
was pointed out by Tsukerblat and co-workers,5 this equation
was introduced phenomenologically by Dzialoshinski to
explain the weak ferromagnetism of R-Fe2O3 and manganese
carbonate crystals.6 The microscopic meaning of the param-
eter G was revealed in the work of Moriya.7 Therefore, the
operator HAS is usually termed the Dzialoshinski-Moriya
antisymmetric (AS) interaction. AS exchange leads to
qualitative and quantitative changes in the temperature and
field dependences of the magnetic susceptibility at low
temperatures. These features are due to the nonlinear
behavior of levels in the magnetic field when AS exchange
is taken into account, and they consist of a reduction of the
magnetic moments.5 Information about Gij values for isolated
complexes is very scarce. The first experimental observation
of the antisymmetric exchange parameter on the electronic
properties of the trinuclear complex [Cu3(µ3-OH)(pyridine-
2-aldoxime)3 (SO4)]‚10.5H2O was made by Tsukerblat and
co-workers.8 Experimental applications of this exchange term
(2) (a) Sowrey, F. E.; Tilford, C.; Wocadlo, S.; Anson, C. E.; Powell, A.
K.; Bennington, S. M.; Montfrooij, W.; Jayasooriya, U. A.; Cannon,
R. D. J. Chem. Soc., Dalton Trans. 2001, 862. (b) Hibbs, W.; van
Koningsbruggen, P. J.; Arif, A. M.; Shum, W. W.; Millar, J. S. Inorg.
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3
as for Fe3+3, and Cr3+ carboxylates.11,12
3
In this work, we describe the synthesis, X-ray structure,
and magnetic properties of two cyclic trimeric compounds:
[Cr3(µ3-O)(µ2-PhCOO)6(H2O)3]NO3‚4H2O‚2CH3OH (1) and
[Cr3(µ3-O) (µ2-PhCOO)2(µ2-OCH2-CH3)2(bpy)2(NCS)3] (2).
Complex 1 shows a similar cationic structure to those already
reported,4k,m-4r but the skeleton of the [Cr3O] core of complex
2 is unique among the structurally characterized (µ3-oxo)-
trichromium(III) complexes.
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11018 Inorganic Chemistry, Vol. 46, No. 26, 2007