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Developments in Ceramic Materials Research

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124<br />

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

7. LOW-TEMPERATURE NEUTRON DIFFRACTION<br />

7.1. B and C type Cr(PO3)3 Metaphosphates<br />

The neutron diffraction petterns at 1.8 K for B and C chromium metaphosphates were<br />

collected <strong>in</strong> the D2B powder diffractometer. The patterns clearly exhibit extra magnetic peaks<br />

<strong>in</strong>dicat<strong>in</strong>g that both compounds are magnetically ordered at 1.8 K. The thermal evolution for<br />

Cr(PO3)3 was followed <strong>in</strong> the D1B <strong>in</strong>strument form 1.8 to 10 K. The results confirm the<br />

presence of a three-dimensional order. The D1B diffraction pattern at 1.8 K shows a better<br />

resolution of the magnetic reflections. The magnetic reflections exhibit low <strong>in</strong>tensities due to<br />

the low order<strong>in</strong>g magnetic temperatures observed <strong>in</strong> these compounds. All magnetic peaks<br />

were <strong>in</strong>dexed with a propagation vector k = (0,0,0) referenced to the RT unit cells, <strong>in</strong>dicat<strong>in</strong>g<br />

that both the magnetic and nuclear unit cells are similar. The possible magnetic structures<br />

compatible with Cc and P21/a crystal symmetries for Cr(PO3)3 and Cr2(P6O18), respectively,<br />

have been deduced with the help of Bertaut’s macroscopic theory [53], which allows one to<br />

determ<strong>in</strong>e the symmetry constra<strong>in</strong>ts between each magnetic moment of the Cr(III) ions<br />

belong<strong>in</strong>g to the same general crystallographic position. The order<strong>in</strong>g of the magnetic<br />

moments compatible with the symmetry operations was determ<strong>in</strong>ed and the agreement<br />

between the observed and calculated diffraction patterns for each possible magnetic structure<br />

was evaluated.<br />

7.1.1. C-Type Cr(PO3)3<br />

The magnetic reflections observed for Cr(PO3)3 can be <strong>in</strong>dexed on the basis of the crystal<br />

unit cell and obey the rules (hkl) wit h+k = 2n (i.e., C-centered mode rema<strong>in</strong>s) and (h0l) with l<br />

= 2n+1 (i.e., forbidden by the c glide plane). It is worth mention<strong>in</strong>g than some of the nuclear<br />

reflections could have magnetic contributions to their <strong>in</strong>tensities. The magnetic atoms occupy<br />

three general 4a different crystallographic sites. The positions <strong>in</strong> the cell of the different<br />

atoms belong<strong>in</strong>g to the Cr(1), Cr(2) and Cr(3) sublattices are numbered 1a, 1b, 1c, 1d; 2a, 2b,<br />

2c 2d and 3a, 3b, 3c, 3d, respectively.<br />

Us<strong>in</strong>g the method developed by Bertaut and tak<strong>in</strong>g <strong>in</strong>to account the restra<strong>in</strong>ts imposed by<br />

symmetry elements of the space group Cc along the three directions x, y and z, the different<br />

possible orientations of the magnetic moments were evaluated. The ref<strong>in</strong>ement of the<br />

components of the magnetic moments gives My = 0, <strong>in</strong>dicat<strong>in</strong>g than they lie <strong>in</strong> the (010)<br />

plane. The best fit of the D1B experimental patterns for Cr(PO3)3 at 1.8 K is plotted <strong>in</strong> Figure<br />

21. The components of the ref<strong>in</strong>ed magnetic moments of Cr(1), Cr(2) and Cr(3) are,<br />

respectively, Mx = 1.7(2) μB and Mz = 1.1(1) μB per chromium ion with a resultant magnetic<br />

moment of 2.58(9) μB per Cr(III) ion. The nuclear and magnetic discrepancy factors are Rp =<br />

3.22, Rwp = 4.58, χ 2 = 18.3, RBragg = 4.35 and Rmag = 23.3. The magnetic structure of Cr(PO3)3<br />

is shown <strong>in</strong> Figure 22. The results are similar to those observed for the Mo(PO3)3 phase,<br />

which was resolved <strong>in</strong> the Ia unit cell, and some chromium phosphates <strong>in</strong> which the magnetic<br />

moments are near 2.4 μB [54,55].<br />

The magnetic structure of the C-type Cr(PO3)3 metaphosphate is consistent with the<br />

presence of (CrO6) octahedra where the magnetic moments are antiferromagnetically ordered<br />

<strong>in</strong> the x direction whereas those along the y and z directions show parallel alignment (see<br />

Figure 22).

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