A low temperature process for converting hematite (α-Fe2O3) thin films into magnetite (Fe3O4is described. The films produced are unambiguously identified as magnetite by several complementary methods of analysis. These include α-backscattering spectrography, X-ray powder diffractometry, and observations of electrical, magnetic, and optical properties.
Published in:
Magnetics, IEEE Transactions on
(Volume:8
,
Issue:
3
)
Date of Publication:
Sep 1972
- Page(s):
-
277
-
278
- ISSN :
-
0018-9464
- Digital Object Identifier :
-
10.1109/TMAG.1972.1067513
- Product Type:
-
Journals & Magazines
- Date of Current Version :
-
06 January 2003
- Issue Date :
-
Sep 1972
- Sponsored by :
-
IEEE Magnetics Society