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Perovskites perovskite intergrowth structures

The cubic AMO3 perovskite structure consists of an MO3 array of comer-shared MO6/2 octahedra with a large A cation at the body-center position. As is illustrated in tig. 1, this structure allows formation of the Ruddlesden-Popper (1957,1958) rock-salt/perovskite intergrowth structures MO (AMO3 ) . In all these structures, the mismatch between the equilibrium (A-O) and (M-O) bond lengths is given by the deviation from unity of the geometric tolerance factor... [Pg.250]

Modular structures are those that can be considered to be built from slabs of one or more parent structures. Slabs can be sections from just one parent phase, as in many perovskite-related structures and CS phases, or they can come from two or more parent structures, as in the mica-pyroxene intergrowths. Some of these crystals possess enormous unit cells, of some hundreds of nanometers in length. In many materials the slab thicknesses may vary widely, in which case the slab boundaries will not fall on a regular lattice and form planar defects. [Pg.198]

Perovskites constitute an important class of inorganic solids and it would be instructive to survey the variety of defect structures exhibited by oxides of this family. Nonstoichiometry in perovskite oxides can arise from cation deficiency (in A or B site), oxygen deficiency or oxygen excess. Some intergrowth structures formed by oxides of perovskite and related structures were mentioned in the previous section and in this section we shall be mainly concerned with defect ordering and superstructures exhibited by these oxides. [Pg.268]

As an example, we briefly describe here the observations made for Laj. Cax-Fe03. In this solid solution system, a single perovskite-brownmillerite intergrowth structure ( = 3) is foimd at composition x = % [224]. The intergrowth structure exhibits ideal stoichiometry, i.e. LaCa2Fe30g, at reduced oxygen partial pressures near the minimum observed in the electrical conductivity [199]. For any other composition, a disordered intergrowth is observed. [Pg.498]

Modules of perovskite-type (abbreviated to perovskite) crystal structure alternating with other structural modules occur in several crystalline materials that are known as hybrid or intergrowth perovskites. Three-dimensional (3D - the octahedra share corners in three non-coplanar directions such that layers of thickness many octahedra are formed), two-dimensional (2D - the octahedra share corners in two directions such that layers of thickness one octahedron are formed), onedimensional (ID - the sharing of octahedral corners develops along one direction only such that rows of octahedra result) and zero-dimensional (OD - only isolated octahedra occur) perovskite layers are known. In the OD and ID layers, the positions of the isolated octahedra (OD) and rows of octahedra (ID) are supposed to match those of the octahedral framework in the perovskite structure. [Pg.370]

In the brownmillerite structure, the oxygen vacancies order in such a way that half the iron of CaFe02.5 are octahedrally coordinated and half are tetrahedrally coordinated. This ordering is an expression of the tetrahedral-site stability of Fe ions. In a system like Lai yCayFe03 x < y/2, there is a tendency to form intergrowths of perovskite and brownmillerite structures the oxygen vacancies do not remain randomly distributed. Mossbauer spectra at 4.2 K for this complex system exhibit three sextets they have been interpreted in terms of 2 Fe and one Fe " ", or of an Fe and the disproportiona-... [Pg.61]


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