Synthesis, structure, and magnetic properties of the low-symmetry tetranuclear cubane-like nickel complex [Ni-4(pypentO)(pym)(mu(3)-OH)(2)(mu-Oac)(2)(NCS)(2)(OH2)]
Jm. Clemente-juan et al., Synthesis, structure, and magnetic properties of the low-symmetry tetranuclear cubane-like nickel complex [Ni-4(pypentO)(pym)(mu(3)-OH)(2)(mu-Oac)(2)(NCS)(2)(OH2)], INORG CHEM, 39(24), 2000, pp. 5515-5519
The terranuclear [Ni-4(pypentO)(pym)(mu (3)-OH)(2)(mu -Oac)2(NCS)(2)(OH)(2)
] cubane-like complex has been prepared, and its structure and magnetic pro
perties have been studied (pypentO and pym are the deprotonated forms of 1,
5-bis[(2-pyridylmethyl)amino]pentane-3-ol and 2-pyridylmethyl, respectively
). The X-ray diffraction analysis of this novel nickel complex (C61H74N14O2
5.5S4Ni8, monoclinic, P2(1), a = 13.9375(14) Angstrom, b = 20.6604(18) Angs
trom, c = 16,6684(19) Angstrom, beta = 110.619(12)degrees, Z = 2) showed a
Ni4O4 cubane arrangement of four nickel atoms, four mu (3)-O bridging ligan
ds (one pypentO, one pym, and two OH-), two syn(-)syn bridging acetates, an
d three terminal monodentate ligands (two NCS- and one OH2). In this low-sy
mmetry elongated cubane, the four Ni-Ni long distances (3.18 Angstrom) corr
espond to the faces of the cube:including two mu (3)-OR bridges, and the tw
o Ni-Ni short distances (2.94 Angstrom) correspond to the faces including t
wo mu (3)-OR and one acetate bridges. The temperature dependence of the mag
netic susceptibility was fitted with J(q) = -3.09 cm(-1), J(2) = 15.0 cm(-1
), J(3) = 6.72 cm(-1), and g = 2.27. The differences in sign among the J(1)
, J(2), and J(3) superexchange interactions is in good agreement with the d
ifferent types of faces present in this Ni4O4 cubane core. The two faces of
the cube, including two mu (3)-OR bridges associated with one acetate brid
ge, exhibit ferromagnetic interactions, while the four faces which include
only mu (3)-OR bridges exhibit antiferromagnetic interactions, The very sma
ll zero field splitting may be attributed to the fact that the ground slate
is diamagnetic. The nature of the ground State is confirmed by the good si
mulation of the magnetization curves at 2 and 5 K (diagonalization of the f
ull matrix taking into account all energy levels obtained with the paramete
r set resulting from the fit of the susceptibility curve). The large differ
ences in J values resulting from small differences in Ni-O-Ni angles in thi
s Ni4O4 core of very low symmetry reflect a quite strong magnetostructural
correlation.