The aim of this letter is to show that a number of experimentally gathered data on magnetic properties of amorphous paramagnetic compounds can be interpreted in terms of a very simple structural model for these systems. To the Authors ' knowledge, the present approach, though only providing a clue to the problem, is applied here for the first time to the case of amorphous compounds. The splitt ing of the free-ion ground state of transit ion metal ions in aggregate systems, and the related magnetic properties, are greatly influenced by the local symmetry of the environment of the ion. The magnetic properties of typical amorphous compounds containing transit ion metal ions can then be interpreted in terms of the symmetry of short-range order structures which are present in these materials, even in the absence of any long-range order. Complex amorphous systems containing relatively large amounts of transit ion metal ions can be, for instance, aluminosilicate (~) or alkaliborate (~) glasses into which transition metal oxides, principally Fe.,0a, are doped. Other amorphous materials can be obtained by inciting and quenching transit ion metal oxides (CoO (a), MR0 (3), Fe20 a (4), Ti02-Ti~08 (~)) with phosphorus pentoxide P~O 5. Typically these compounds show a paramagaetic behaviour down to 4 K. In some cases only a partial amorphicity of the compound can be obtained. This feature can be controlled by inspection through X-ray diffraction and also by comparison of the magnetic behaviour of samples with crystalline ones with similar compositions. In any case, a large part of the obtained compounds arc definitely in complete amorphous phase within the limits of experimental techniques.
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