Single-phase perovskites in the solid solution series La 0.7+y A 0.3-y Mn 1-x M x O 3 (with 0.00 e x e 0.10; A ) Sr 2+ , M ) Cu 2+ , Zn 2+ , Sc 3+ , Cr 3+ , Co 3+ , and Ga 3+ ; A ) Ba 2+ , M ) Cu 2+ , Zn 2+ , and Sc 3+ ) have been prepared via the acetic acid solutions freeze-drying method. This soft procedure makes possible strict stoichiometric control, and the synthetic variables allow one to maintain a constant proportion of Mn 4+ (ca. 32%) in the 47 compounds prepared. In this way, the concentration of cationic vacancies at A and B sites is practically negligible in all cases. X-ray powder diffraction patterns corresponding to the 47 compounds have been completely indexed with rhombohedral perovskite cells. The crystal structures have been refined in space group R h 3c, in the hexagonal setting, from room-temperature data. The variation with x of a set of structural parameters (rhombohedral cell volume, rhombohedral cell angle, and B-O and A-O bond lengths) has been considered as a function of the mean sizes of cations at A and B sites. Manganates in these series present colossal magnetoresistance. The values of the critical temperature, T c , for the paramagnetic-ferromagnetic transition in La 0.7+y A 0.3-y Mn 1-x M x O 3 exhibit three different patterns, which clearly appear related to the mean size of cations at B sites. This fact has been interpreted by considering the variation of the electronic contribution to T c with the structural disorder introduced by the presence of cations with different sizes at B sites.
Single-phase perovskites in the solid solution series
La1
-
x
Na
x
MnO3+
δ
have been obtained
using a soft treatment, which makes possible strict stoichiometric
control. Under these
conditions, it becomes possible to systematically study the influence
of the sodium content
on the electronic properties of materials in this series. As long
as all the samples have
practically the same Mn4+ content (33%), the number of
vacancies at A and B sites of the
perovskite structure depends on the sodium content, and it decreases as
x increases.
Susceptibility to alternating current, magnetization, resistivity,
and magnetoresistivity
measurements have allowed us to establish relevant points of the
electronic phase diagram
of this alkali-metal-doped lanthanide manganate system. These
results, together with those
previously obtained for
La1
-
x
K
x
MnO3+
δ,
reveal the existence of a correlation between the
critical temperature for ferromagnetic ordering and the concentration
of vacancies at the B
sites, v
B, in samples with a fixed concentration
of Mn4+. Such a correlation can be
understood
in terms of a magnetic phase segregation model in which the materials
are thought of as
composed by clusters, formed by the vacancies (trapping centers for
mobile holes) and
neighboring Mn cations (on which holes are trapped), and a matrix,
formed by the remaining
Mn cations. Within this model, the decrease in the number of
mobile holes in the matrix is
the cause of the decrease in the critical temperature with
v
B.
Series of perovskite oxides with the composition LaMn 12x M x O 3zd (M~Cr, Co; 0¡x¡1) have been synthesized by thermal treatment of precursors obtained by freeze-drying of acetic acid solutions. The oxides have been characterized by X-ray diffraction, and the Mn 4z content and, thus, the oxygen excess, d, has been determined by redox back-titration. LaMnO 3.14 and LaCrO 3 phases have the rhombohedral-LaAlO 3 and the orthorhombic-GdFeO 3 structures, respectively. The LaMn 12x Cr x O 3zd phases have the rhombohedral structure for x¡0.3, and the orthorhombic structure for x¢0.5. LaCoO 3 has, as LaMnO 3.14 , the rhombohedral structure. However, the LaMn 12x Co x O 3zd phases have orthorhombic structure for 0.05¡x¡0.55. The evolution of the crystal symmetry has been interpreted by considering the effect of the size of the substituting ion on the capability of the perovskite network to accommodate the oxygen excess (d).
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