Abstract
We investigated the charge distribution in rare-earth (R=La, Nd, Sm) doped hexaferrites RxSr1-xFe12O19 at x less than or equal to 0.33 T = 4.2 K and in magnetic fields up to 7 T with the local probe of Fe-57- nuclear magnetic resonance (NMR). All five crystallographic Fe-sites in the doped material are subject to an additional internal field DeltaB(hf), independent of R. DeltaB(hf) increases to 0.4 T with x less than or equal to 0.06, then decreases again. For x > 0.15, the Fe-spectrum is nearly indistinguishable from the one observed in undoped samples. The homogeneous shift of all Fe-lines is ascribed to the formation of large polarons with a magnetic polarization increasing at small x, and decreasing again when additional states are involved in their formation. (C) 2003 Elsevier B.V. All rights reserved.
| Original language | English |
|---|---|
| Pages (from-to) | 2219-2220 |
| Number of pages | 2 |
| Journal | Journal of Magnetism and Magnetic Materials |
| Volume | 272-276 |
| Issue number | 3 |
| Publication status | Published - 1 Jan 2004 |
Keywords
- NMR
- hexaferrites
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