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Spontaneous magnetization curve of $$alpha$$-iron at high pressures determined using ${it in situ}$ neutron diffraction

Aoki, Katsutoshi*; Takano, Masahiro*; Fukuyama, Ko*; Kagi, Hiroyuki*; Machida, Akihiko*; Saito, Hiroyuki*; Hattori, Takanori   ; Sano, Asami   ; Funakoshi, Kenichi*

The temperature dependence of the magnetic moment of bcc $$alpha$$-iron was investigated over the range 300-950 K at pressures of approximately 2 and 6 GPa by ${it in situ}$ neutron powder diffraction. The $$^{54}$$Fe isotope, whose neutron scattering length is approximately half that of naturally abundant Fe, was employed to enhance the relative contribution of magnetic scattering. Curie temperatures ($$T_{rm{C}}$$) were determined to be 946(30) K, 838(50) K and 740(40) K at 2.1, 6.0 and 6.7 GPa, respectively, defining a magnetic phase boundary described by $$T_{rm{C}}$$(K) = 1043 - 49(7)$$P$$ + 1.3(1.2)$$P^2$$. Upon heating at 6.7 GPa, the $$alpha-gamma$$ structural transition was observed to follow the magnetic transition. This transition sequence indicates that the magnetic phase boundary lies on the low-temperature side of the $$alpha-gamma$$ phase boundary. Accordingly, the $$alpha-gamma$$ transition corresponds to a structural transformation from paramagnetic bcc to paramagnetic fcc iron.

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Category:Materials Science, Multidisciplinary

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