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Updated: Jan 9, 2026

Methods of Ex Situ and In Situ Investigations of Structural Transformations: The Case of Crystallization of Metallic Glasses
Published on: June 7, 2018
Higher Dimensionality in the Mg-Co-B System: Synthesis and Structure of Incommensurate Composite Mg1+εCo4B4
Paul Oftedahl1, Gourab Bhaskar1, Nawsher J Parvez2
1Department of Chemistry, Iowa State University, Ames, Iowa 50011, United States.
Abstract:
Guided by high-temperature in situ X-ray diffraction, the discovery and synthesis of Mg1+εCo4B4 (ε ≈ 0.272) using a MgH2 hydride precursor is reported, along with a detailed crystal structure description and measurement of magnetic properties. The mismatch in lattice periodicities between Mg and Co-B substructures places Mg1+εCo4B4 in the family of incommensurate composite crystals and prompted structural refinement in a (3 + 1)-dimensional model. The structure of Mg1+εCo4B4 (P42/ncm(00γ)s00s, a = 6.75847(7) Å, c = 3.94007(8) Å, q = (0, 0, 1.2721(3))) was refined from neutron powder diffraction and high-resolution powder X-ray diffraction data and confirmed by scanning transmission electron microscopy and electron diffraction. Mg1+εCo4B4 is isostructural to Nd1+εFe4B4 and several related ternary borides with 0.07 ≤ ε ≤ 0.17, with Mg occupying the rare-earth site. Satellite reflections in the electron diffraction patterns hinted at positional modulation of the transition metal-boron substructure by Mg atoms, but this could not be refined from the neutron or X-ray diffraction data. Low-temperature magnetic measurements show no indications of long-range magnetic ordering or superconductivity down to 5 K. DFT calculations confirmed the absence of a magnetically ordered ground state and the stability of a 5:4 supercell (ε = 0.25) relative to the fully commensurate structure. Neutron diffraction and synthesis from elemental Mg demonstrated that Mg1+εCo4B4 is not a hydrogen-stabilized phase. Mg1+εCo4B4 represents the second compound reported in the Mg-Co-B system and the first superspace symmetry model of a Nd1+εFe4B4-type incommensurate composite compound refined from powder diffraction data.
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