Please use this identifier to cite or link to this item: https://libjncir.jncasr.ac.in/xmlui/handle/10572/921
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dc.contributor.authorMahesh, R-
dc.contributor.authorMahendiran, R-
dc.contributor.authorRaychaudhuri, A K-
dc.contributor.authorRao, C N R-
dc.date.accessioned2012-11-06T11:01:54Z-
dc.date.available2012-11-06T11:01:54Z-
dc.date.issued1995-11-15-
dc.identifier0022-4596en_US
dc.identifier.citationJournal of Solid State Chemistry 120(1), 204–207 (1995)en_US
dc.identifier.urihttps://libjncir.jncasr.ac.in/xmlui/10572/921-
dc.descriptionLetter. Restricted Access.en_US
dc.description.abstractBased on an extensive study of a large variety of rare earth manganates (rare earth = La, Nd, Gd, or Y) with Ca, Sr, Ba, and Pb as the substituents, as well as of LaMnO3 samples with varying Mn4+ content, it is shown that the ferromagnetic transition temperature, Tc, as well as the insulator-metal (I-M) transition temperature, Tp , increases with the weighted average radius of the A-cations, 〈rA〉, showing a maximum at 1.23 ± 0.01 Å. The essentially linear region (〈rA〉 = 1.18-1.24 Å) demarcates the ferromagnetic metal and paramagnetic insulator regimes. The peak resistivity at the I-M transition, as well as the magnitude of the magnetoresistance (MR), decreases with increasing 〈rA〉. Only below a 〈rA〉 of 1.23 ± 0.01 Å is the MR greater than 50%.en_US
dc.description.urihttp://dx.doi.org/ 10.1006/jssc.1995.1398en_US
dc.language.isoenen_US
dc.publisherAcademic Press Inc JNL Comp Subscriptionsen_US
dc.rights© 1995 Academic Press Incen_US
dc.subjectA-Site Cationsen_US
dc.subjectGiant Magnetoresistanceen_US
dc.subjectDoped Rare Earth Manganatesen_US
dc.subjectferromagnetic transition temperatureen_US
dc.subjectparamagnetic insulator regimesen_US
dc.titleEffect of the Internal Pressure Due to the A-Site Cations on the Giant Magnetoresistance and Related Properties of Doped Rare Earth Manganates, Ln1-xAxMnO3 (Ln = La, Nd, Gd, Y; A = Ca, Sr, Ba, Pb)en_US
dc.typeArticleen_US
Appears in Collections:Research Papers (Prof. C.N.R. Rao)

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