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Nanomagnetic properties of the meteorite cloudy zone
Joshua F Einsle1,2, Alexander S Eggeman3, Ben H Martineau2
1Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, United Kingdom; jfe26@cam.ac.uk.
Summary
Meteorites record magnetic history in nanoscale tetrataenite intergrowths. This study reveals the 3D structure and magnetic recording mechanism of the cloudy zone, offering insights for paleomagnetism and sustainable magnets.
Area of Science:
- * Planetary Science
- * Materials Science
- * Geophysics
Background:
- * Meteorites preserve thermal and magnetic histories through mineral intergrowths.
- * The
- cloudy zone
- in meteorites contains tetrataenite, a ferromagnetic mineral with potential as a sustainable magnet alternative.
- * Understanding tetrataenite's nanostructure is key to its magnetic applications.
Purpose of the Study:
- * To elucidate the 3D architecture of the meteorite cloudy zone at subnanometer resolution.
- * To model the mechanism of remanence acquisition during slow cooling.
- * To assess the paleomagnetic utility and potential for synthetic magnet development.
Main Methods:
- * High-resolution electron diffraction and tomography.
- * Atom probe tomography (APT).
- * Micromagnetic simulations.
Main Results:
- * Revealed isolated tetrataenite islands in an ordered superstructure matrix.
- * Identified clustering of three crystallographic variants influencing magnetic encoding.
- * Modeled remanence acquisition via magnetic domain state transformations driven by Fe-Ni ordering at 320 °C.
- * Determined that coarse and intermediate cloudy zones are suitable for paleomagnetism, while fine regions mimic rare-earth magnets.
Conclusions:
- * The cloudy zone records a coherent paleomagnetic snapshot at 320 °C.
- * Specific regions of the cloudy zone are valuable for paleomagnetic studies.
- * Fine-grained tetrataenite offers a pathway for developing synthetic permanent magnets.
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