Jl. Mesa et al., Structure and magnetic properties of Li3Fe2(AsO4)(3-x)(PO4)(x) [x=0, 1, 1.5, 2]: two sublattice weak ferromagnets, J MAT CHEM, 10(12), 2000, pp. 2779-2785
The Li3Fe2(AsO4)(3 - x)(PO4)(x) (x = 0, 1, 1.5, 2) solid solution was prepa
red by the ceramic method. Li3Fe2(AsO4)(3) crystallizes in the monoclinic P
112(1)/n space group with the cell parameters, a = 8.608(1), b = 12.215(1),
c = 8.929(1) Angstrom and gamma = 90.76(1)degrees. The structure consists
of a three-dimensional framework of vertex-sharing FeO6 octahedra and AsO4
tetrahedra with the lithium ions distributed in three four-coordinated crys
tal sites. There are two independent iron positions in the structure of thi
s compound, Fe(1) and Fe(2). The cell parameters of the isostructural Li3Fe
2(AsO4)(3 - x)(PO4)(x) (x = 0, 1, 1.5, 2) phases follow Vegard's law. The I
R spectra show the evolution of the intensity for the bands corresponding t
o the AsO4 and PO4 tetrahedra in the solid solution. An isotropic signal wi
th a g value of 2.0 is observed in the ESR spectra of all compounds, in goo
d agreement with the presence of a high spin Fe(III) ion with slightly dist
orted octahedral symmetry. The magnetization measurements and the magnetic
DC and AC susceptibility data show an antiferromagnetic behavior for these
compounds, with the presence of a ferromagnetic component below the orderin
g temperature. T-N decreases from 35.5 to 31 K with decreasing the amount o
f arsenate. The magnetic results are explained by the existence of a phenom
enon of ferrimagnetism in these compounds, due to the existence of two diff
erent magnetic sublattices, corresponding to the Fe(1) and Fe(2) sites. The
presence of canting between the magnetic moments of these two sublattices
has been also detected. This fact agrees with the relative orientation of t
he FeO6 magnetic octahedra in the Li3Fe2(AsO4)(3 - x)(PO4)(x) (x = 0, 1, 1.
5, 2) compounds.