Please use this identifier to cite or link to this item: https://doi.org/10.1088/0022-3727/41/20/205001
Title: Microstructural and magnetic properties of L10 FePt-C (0 0 1) textured nanocomposite films grown on different intermediate layers
Authors: Chen, J.S. 
Lim, B.C.
Hu, J.F.
Ding, Y.F.
Chow, G.M. 
Ju, G.
Issue Date: 21-Oct-2008
Citation: Chen, J.S., Lim, B.C., Hu, J.F., Ding, Y.F., Chow, G.M., Ju, G. (2008-10-21). Microstructural and magnetic properties of L10 FePt-C (0 0 1) textured nanocomposite films grown on different intermediate layers. Journal of Physics D: Applied Physics 41 (20) : -. ScholarBank@NUS Repository. https://doi.org/10.1088/0022-3727/41/20/205001
Abstract: The FePt : C films with different volume fractions of carbon and different thicknesses were epitaxially grown on a CrRu(2 0 0) underlayer with Pt and MgO intermediate layers. The magnetic properties and microstructure of these FePt : C films were investigated. The FePt : C films grown on the Pt intermediate layer consisted of a continuous layer of FePt, with overlying granular FePt grains, while the FePt : C films grown on the MgO intermediate layer consisted of granular FePt : C layers with overlying granular grains. The formation of the overlying granular FePt grains was attributed to carbon diffusion to the surface which resulted in the second nucleation of FePt. The different interface energies and surface energies of FePt on Pt and MgO intermediate layers caused the formation of an initial continuous FePt layer on the Pt intermediate layer and initial granular FePt layers on the MgO intermediate layer. The coupling between the continuous FePt layer or the granular FePt layer and the overlying granular FePt grains resulted in simultaneous magnetization reversal and thus strong exchange coupling in FePt : C films. © 2008 IOP Publishing Ltd.
Source Title: Journal of Physics D: Applied Physics
URI: http://scholarbank.nus.edu.sg/handle/10635/86540
ISSN: 00223727
DOI: 10.1088/0022-3727/41/20/205001
Appears in Collections:Staff Publications

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