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Related Concept Videos

Ferromagnetism01:31

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Materials like iron, nickel, and cobalt consist of magnetic domains, within which the magnetic dipoles are arranged parallel to each other. The magnetic dipoles are rigidly aligned in the same direction within a domain by quantum mechanical coupling among the atoms. This coupling is so strong that even thermal agitation at room temperature cannot break it. The result is that each domain has a net dipole moment. However, some materials have weaker coupling, and are ferromagnetic at lower...
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Metallic solids such as crystals of copper, aluminum, and iron are formed by metal atoms. The structure of metallic crystals is often described as a uniform distribution of atomic nuclei within a “sea” of delocalized electrons. The atoms within such a metallic solid are held together by a unique force known as metallic bonding that gives rise to many useful and varied bulk properties.
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Color in Coordination Complexes
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Methods of Ex Situ and In Situ Investigations of Structural Transformations: The Case of Crystallization of Metallic Glasses
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Accelerating Nature: Induced Atomic Order in Equiatomic FeNi.

Laura H Lewis1, Plamen S Stamenov2

  • 1Department of Chemical Engineering and Department of Mechanical and Industrial Engineering, Northeastern University, Boston, MA, 02115, USA.

Advanced Science (Weinheim, Baden-Wurttemberg, Germany)
|December 10, 2023
PubMed
Summary
This summary is machine-generated.

Researchers produced atomically ordered iron-nickel (FeNi), or tetrataenite, in bulk samples. Further processing could enhance its properties for advanced permanent magnets, crucial for green energy solutions.

Keywords:
Mössbauer spectroscopychemical ordermeteoritespermanent magnetsphase transitions

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Area of Science:

  • Materials Science
  • Solid State Physics
  • Mineralogy

Background:

  • Atomically ordered FeNi, known as tetrataenite, is a naturally occurring mineral found in meteorites.
  • Understanding its formation and properties is key to developing advanced magnetic materials.

Purpose of the Study:

  • To confirm the production of atomically ordered FeNi (tetrataenite) in bulk samples.
  • To quantify the amount of tetrataenite formed under specific processing conditions.
  • To compare the atomic order of processed FeNi with natural tetrataenite.

Main Methods:

  • Simultaneous conversion X-ray and backscattered γ-ray 57 Fe Mössbauer spectroscopy.
  • Thermal treatment of FeNi alloys under simultaneous magnetic and stress fields for 6 weeks.
  • Analysis of precursor and processed alloy samples.

Main Results:

  • Up to 22% tetragonal tetrataenite was quantified in processed FeNi samples; the remainder was cubic FeNi alloy.
  • Processed FeNi showed a lower degree of atomic order compared to meteoritic tetrataenite.
  • Meteoritic tetrataenite exhibited low uniaxial magnetocrystalline anisotropy energy (≈1 kJ·m-3).

Conclusions:

  • Targeted refinements in FeNi processing can enhance atomic order and magnetocrystalline anisotropy.
  • Improved FeNi could lead to enhanced magnetic energy products for permanent magnets.
  • Tetrataenite shows potential for advanced permanent magnet applications, supporting green energy initiatives.