1977
DOI: 10.1016/0304-8853(77)90107-x
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Antiferromagnetism of FCC Fe thin films

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1986
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Cited by 28 publications
(6 citation statements)
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“…In Cu precipitates γ-iron can be stabilized till very low temperatures, which allows studying its low-temperature magnetic properties. Early experimental studies have shown that this substance is a weak itinerant antiferromagnet with the Neel temperature of the order of 100 K [4][5][6]. Later it was found [7][8][9] that the corresponding incommensurate wave vector Q ≈ 2π(1, 0.13, 0) in units of inverse lattice parameter a is close to the so called AFM-I magnetic structure.…”
Section: Introductionmentioning
confidence: 90%
“…In Cu precipitates γ-iron can be stabilized till very low temperatures, which allows studying its low-temperature magnetic properties. Early experimental studies have shown that this substance is a weak itinerant antiferromagnet with the Neel temperature of the order of 100 K [4][5][6]. Later it was found [7][8][9] that the corresponding incommensurate wave vector Q ≈ 2π(1, 0.13, 0) in units of inverse lattice parameter a is close to the so called AFM-I magnetic structure.…”
Section: Introductionmentioning
confidence: 90%
“…Antiferromagnet ordering in g (FCC) Fe thin films [12][13][14], g (FCC) Fe precipitates in Cu and 304 stainless steel [10] (all are paramagnetic at room temperature (RT) and show a single line M .…”
Section: Introductionmentioning
confidence: 99%
“…The N! eel temperature (T N ) in these materials was determined using either the ''thermal scan'' method [10,12], or by measuring the linewidth as a function of temperature [13,14].…”
Section: Introductionmentioning
confidence: 99%
“…The weakening of the main ESR lines, g 1 and g 2 , with decreasing temperature indicates the emergence of an anisotropic antiferromagnetic (AF) order at a Néel temperature T N ≈ 260 K (Figure b). An AF order with a Néel temperature T N up to 100 K was reported for γ‐Fe thin films with face‐centered cubic (fcc) crystal symmetry obtained by epitaxial growth or precipitation, an AF order can emerge when bcc γ‐Fe undergoes a crystal phase transition to fcc below a critical layer thickness due to stronger magnetic interactions arising from a smaller lattice constant and/or surface effects; AF and FM orders can also coexist within an Fe‐cluster due to its composite crystal structure . The coexistence of different magnetic phases in our system may arise from nonequivalent Fe‐atoms in the islands and strain effects at the interface with the diamagnetic InSe, which requires further investigation.…”
mentioning
confidence: 70%