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Developments in Ceramic Materials Research

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100<br />

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

metaphosphate wavelengths of 2.41 Å (D2B) at 2 K were used <strong>in</strong> order to obta<strong>in</strong> a better<br />

resolution of the magnetic data at lower angles. D1B has a 400 element l<strong>in</strong>ear multidetector<br />

cover<strong>in</strong>g an angular range of 80 °. High flux and medium resolution of D1B at 2.52 Å were<br />

used to study the thermal evolution of Fe(PO3)3 <strong>in</strong> the temperature range 1.5 – 20 K to resolve<br />

the magnetic contributions of the neutron patterns. The magnetic and nuclear structures were<br />

ref<strong>in</strong>ed simultaneously, tak<strong>in</strong>g as start<strong>in</strong>g parameter of each pattern those result<strong>in</strong>g from the<br />

ref<strong>in</strong>ement of the preced<strong>in</strong>g one. A pseudo-Voigth function was chosen to generate the l<strong>in</strong>e<br />

shape of the diffraction peaks.<br />

4. RESULTS AND DISSCUSION<br />

4.1. Nuclear Crystal Structure Description<br />

The M(PO3)3 (M= Ti, V, Cr, Mo and Fe) metaphosphates are the most condensed<br />

phosphate systems where the metal ions present the unusual +3 oxidation state [5-10]. For<br />

these compounds, the crystal structure may be described as formed by isolated (MO6)<br />

octahedra l<strong>in</strong>ked through (PO3)∞ cha<strong>in</strong>s of (PO4) tetrahedra (see Figure 1a). Each (MO6)<br />

group is bridged to six neighbour<strong>in</strong>g (MO6) octaedra by phosphate groups and each<br />

octahedron shares it six apices with different (PO4) tetrahedra. These tetrahedra lie <strong>in</strong> adjacent<br />

layers and lead to a three-dimensional network, <strong>in</strong> which the metallic cations occupy three<br />

different crystallographic positions for every metallic center.<br />

The crystal structure for the other chromium phase, namely the hexametaphosphate, is<br />

formed by (CrO6) octahedra l<strong>in</strong>ked through (PO4) tetrahedra belong<strong>in</strong>g to (P6O18) 6- cycles<br />

(see Figure 1b). The (CrO6) coord<strong>in</strong>ation polyhedra are not vertex- or edge-shared, and are<br />

isolated by (PO4) tetrahedra. Each (CrO6) octahedron <strong>in</strong>teracts with four (P6O18) 6- cycles,<br />

three phosphorous atoms lie <strong>in</strong> the plane def<strong>in</strong>ed by the Cr(III) ions and the other three are<br />

place below and above of the metallic cations <strong>in</strong> a perpendicular plane, lead<strong>in</strong>g to a threedimensional<br />

network [14].<br />

a<br />

Figure 1 (Cont<strong>in</strong>ued).<br />

b c

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