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    Spontaneous magnetization curve of α-iron at high pressures determined using in situ neutron diffraction

    Katsutoshi Aoki1,*, Masahiro Takano1, Ko Fukuyama1,†, Hiroyuki Kagi1, Akihiko Machida2, Hiroyuki Saitoh2, Takanori Hattori3, Asami Sano-Furukawa3, and Ken-ichi Funakoshi4

    • *Contact author: k-aoki@eqchem.s.u-tokyo.ac.jp
    • †Present address: Department of Earth and Planetary Sciences, Graduate School of Science, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka 819-0395, Japan.

    Phys. Rev. B 113, 184440 – Published 11 May, 2026

    DOI: https://doi.org/10.1103/vdnz-y1nk

    Abstract

    The temperature dependence of the magnetic moment of bcc α-iron was investigated over the range 300–950 K at pressures of approximately 2 and 6 GPa by in situ neutron powder diffraction. The Fe54 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 (TC) 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 TC(K)=1043−49(7)P+1.3(1.2)P2. Upon heating at 6.7 GPa, the α–γ 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 α–γ phase boundary. Accordingly, the α–γ transition corresponds to a structural transformation from paramagnetic bcc to paramagnetic fcc iron.

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