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Developments in Ceramic Materials Research

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98<br />

José M. Rojo, José L. Mesa and Teófilo Rojo<br />

giromagnetic tensor that depends of the nature of the metal and of its S-number of sp<strong>in</strong>.<br />

The magnetic study <strong>in</strong>dicates the existence of antiferromagnetic <strong>in</strong>teractions <strong>in</strong> the<br />

majority of the compounds, be<strong>in</strong>g detected for several metaphosphates a weak<br />

ferromagnetic sp<strong>in</strong> cant<strong>in</strong>g phenomenon at low temperatures. In the case of the Ti(III) a<br />

ferromagnetic behavior has been observed. The values of the J-exchanger parameter have<br />

been calculated us<strong>in</strong>g the Rushbrooke and Wood equations for 3D-antiferromagnetic<br />

lattices with different values of the sp<strong>in</strong>. In some case, the D-zero field splitt<strong>in</strong>g<br />

parameter has been calculated from the simultaneously comb<strong>in</strong>ation of the ESR and<br />

susceptibility measurements. The neutron powder diffraction study of the M(PO3)3 (M III =<br />

Cr, Mo and Fe) metaphosphates shows antiferromagnetic structures.<br />

1. INTRODUCTION<br />

The study of phosphates of transition elements with low oxidation states has received<br />

great <strong>in</strong>terest <strong>in</strong> recent years. These compounds exhibit <strong>in</strong>terest<strong>in</strong>g properties such as<br />

magnetic, heterogeneous catalysis, ionic exchange, etc., with potential applications [1,2]. In<br />

this way, the M(PO3)3 materials are <strong>in</strong>terest<strong>in</strong>g ow<strong>in</strong>g to the activity of Cr-conta<strong>in</strong><strong>in</strong>g<br />

alum<strong>in</strong>ophosphates (CrAPO-5 materials) which are well known for their catalytic<br />

performance [3, 4].<br />

The M(PO3)3 (M= Al, Sc, Ti, V, Mo, Rh, Ru,…) metaphosphates are the most condensed<br />

phosphate systems <strong>in</strong> which the metal ions present unusual oxidation states [5-10]. We are<br />

center<strong>in</strong>g this work on the M III = Ti, V, Cr, Mo and Fe, metallic cations, which exhibit some<br />

of them an unusual +III reduced oxidation state <strong>in</strong> their metaphosphate compounds. In the<br />

molybdenum and vanadium metaphosphates only one crystall<strong>in</strong>e phase, the monocl<strong>in</strong>ic Ctype<br />

[M(PO3)3] structure, has been isolated and the structures have recently been reported<br />

[9,10]. However, six different polymorph phases denoted A, B, C, D, E and F have been<br />

described <strong>in</strong> chromium and iron metaphosphates [11,12] but, to our knowledge, the crystal<br />

structures of only two phases (B and C) are known [13-15]. One of them adopts the C-type<br />

[Cr(PO3)3] structure and is characterized by one-dimensional <strong>in</strong>f<strong>in</strong>ite metaphosphate (PO3)∞<br />

cha<strong>in</strong>s and isolated (CrO6) octahedra. The superstructure found <strong>in</strong> s<strong>in</strong>gle crystals X-ray<br />

<strong>in</strong>vestigations for this Cr(PO3)3 structure type, <strong>in</strong> which the monocl<strong>in</strong>ic y axis is tripled, could<br />

be the responsible of the three crystallographic different (CrO6) octahedral units of almost<br />

ideal geometry [13]. The reason for this subcell effect is not immediately apparent <strong>in</strong> this<br />

complex structure and could be necessary to perform an analysis of the symmetry <strong>in</strong> order to<br />

elucidate any translational pseudosymmetry that may occur via concerted polyhedral rotation<br />

[7]. The crystal structure for the other chromium phase, B-type [Cr(PO3)3], namely the<br />

hexametaphosphate Cr2(P6O18), is formed by (CrO6) octahedra l<strong>in</strong>ked through (PO4)<br />

tetrahedra belong<strong>in</strong>g to (P6O18) 6- cycles.<br />

Tak<strong>in</strong>g <strong>in</strong>to account the structural features of these compounds and the nature of the<br />

metallic cations, their magnetic properties are expected to be very <strong>in</strong>terest<strong>in</strong>g. In this way, the<br />

magnetic study of these compounds reveals different types of magnetic exchange <strong>in</strong>teractions,<br />

which range from antiferromagnetic to ferromagnetic for the chromium, molybdenum or iron<br />

phases and the titanium compound, respectively. In the vanadium metaphosphate, the<br />

magnetic behavior is determ<strong>in</strong>ed by both the antiferromagnetic <strong>in</strong>teractions and the zero-field<br />

splitt<strong>in</strong>g parameter characteristic of this cation. To understand the magnetic structures <strong>in</strong> the

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