| dc.contributor.author | Bhosale, D.N. | |
| dc.contributor.author | Verenkar, V.M.S. | |
| dc.contributor.author | Rane, K.S. | |
| dc.contributor.author | Bakare, P.P. | |
| dc.contributor.author | Sawant, S.R. | |
| dc.date.accessioned | 2015-06-03T07:13:34Z | |
| dc.date.available | 2015-06-03T07:13:34Z | |
| dc.date.issued | 1999 | |
| dc.identifier.citation | Materials Chemistry and Physics. 59(1); 1999; 57-62. | en_US |
| dc.identifier.uri | http://dx.doi.org/10.1016/S0254-0584(99)00028-0 | |
| dc.identifier.uri | http://irgu.unigoa.ac.in/drs/handle/unigoa/1040 | |
| dc.description.abstract | Cu(0.5-x)MxZn0.5Fe2O4 ferrites were synthesised by thermal decomposition of oxalate complexes by co-precipitation technique using oxalate precursors. X-ray diffraction studies revealed a single spinel phase with un-detectable impurity phases. Lattice parameter showed a decreasing trend with increasing Mg2+ content, which is attributed to the ionic sizes of Mg2+ and Cu2+ ions. The temperature variation of susceptibility for oxalate complex decomposed at 600 degrees C did not exhibit peak in chi(ac) to T variation. Ferrites with x less than 0.4 sintered at 950 degrees C showed small peak in chi(ac) to T near T-c. However chi(ac) to T variation for the ferrites sintered at 1000 degrees C exhibited MD type grains in predominance. The domain wall width increases with the addition of Mg2+ content. Particle size distribution (PSD) indicated absence of fine particles predominantly. Therefore double T behaviour is not exhibited by the samples. Initial permeability and initial susceptibility increase with increase in Mg2+ content. | en_US |
| dc.publisher | Elsevier | en_US |
| dc.subject | Chemistry | en_US |
| dc.title | Initial susceptibility studies on Cu-Mg-Zn ferrites | en_US |
| dc.type | Journal article | en_US |
| dc.identifier.impf | y |