Abstract
The properties of a magnetically ordered buried Fe oxide layer are presented. This oxide has a room-temperature magnetization exceeding that of [Formula presented] by 42% and of [Formula presented] by 89%. The oxide consists of a component (70%) with a net moment of [Formula presented] ion, while the remaining spins yield no net moment. The oxide magnetization is stabilized in part by the proximate Fe metal.
Original language | English (US) |
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Journal | Physical Review Letters |
Volume | 91 |
Issue number | 26 |
DOIs | |
State | Published - 2003 |
ASJC Scopus subject areas
- General Physics and Astronomy