A program has been initiated to develop
FeIII/oxo cluster
chemistry with the “pseudocarboxylate” ligand dimethylarsinate
(Me2AsO2
–) for comparison
with the well investigated FeIII/oxo/carboxylate cluster
area. The synthesis and characterization of three polynuclear FeIII complexes are reported, [Fe12O4(O2CtBu)8(O2AsMe2)17(H2O)3]Cl3 (1), Na2[Fe12Na2O4(O2AsMe2)20(NO3)6(Me2AsO2H)2(H2O)4](NO3)6 (2), and [Fe3(O2AsMe2)6(Me2AsO2H)2(hqn)2](NO3) (3), where hqnH is 8-hydroxyquinoline.
The Fe12 core of 1 is a type never previously
encountered in FeIII carboxylate chemistry, consisting
of two Fe6 units each of which comprises two {Fe3(μ3-O2–)} units bridged by three
Me2AsO2
– groups and linked
into an Fe12 loop structure by two anti–anti η1:η1:μ Me2AsO2
– groups, a bridging mode extremely rare
with carboxylates. 2 also consists of two Fe6 units, differing in their ligation from those in 1,
and this time linked together into a linear structure by a central
{Na2(NO3)2} bridging unit. 3 is a linear Fe3 complex with no monatomic bridges
between FeIII ions, a very rare situation in FeIII chemistry with any ligands and unprecedented in Fe carboxylate chemistry.
The distinct differences observed in arsinate vs carboxylate ligation
modes are rationalized largely based on the greater basicity of the
former vs the latter. Variable-temperature dc and ac magnetic susceptibility
data reveal all Fe2 pairwise interactions to be antiferromagnetic.
For 1 and 2, the different J
ij
couplings were estimated by use of
a magnetostructural correlation for high nuclearity FeIII–oxo clusters and by density functional theory calculations
using broken symmetry methods, allowing identification of their relative
spin vector alignments and thus rationalization of their S = 0 ground states. The J
ij
values were then used as input values to give excellent fits
of the experimental χM
T vs T data. For 3, the fits of the experimental
χM
T vs T data to
the Van Vleck equation or with PHI gave a very weak J
12 = −0.8(1) cm–1 (H = −2JŜ
i
·Ŝ
j
convention)
between adjacent FeIII ions and an S = 5/2 ground state. These initial FeIII arsinate complexes also provide structural parameters that help
validate literature assignments of arsinate binding modes to iron
oxide/hydroxide minerals as part of environmental concerns of using
arsenic-containing herbicides in agriculture.