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Updated: Mar 26, 2026

Methods of Ex Situ and In Situ Investigations of Structural Transformations: The Case of Crystallization of Metallic Glasses
Published on: June 7, 2018
The low-temperature crystal structure of the multiferroic melilite Ca2CoSi2O7.
Andrew Sazonov1, Vladimir Hutanu1, Martin Meven1
1Institute of Crystallography, RWTH Aachen University, Aachen, Germany.
Calcium cobalt silicate (Ca2CoSi2O7) shows strong magnetoelectric coupling below 5.7 K. Neutron diffraction revealed its low-temperature orthorhombic structure, essential for understanding this multiferroic phase.
Area of Science:
- Solid-state physics
- Crystallography
- Magnetism
Background:
- Ca2CoSi2O7 exhibits multiferroic properties with strong magnetoelectric coupling below TN ≃ 5.7 K.
- Understanding the crystal structure is crucial for theoretical descriptions of the multiferroic phase.
Purpose of the Study:
- To determine the precise crystal structure of Ca2CoSi2O7 in its antiferromagnetic ground state.
- To provide structural data for symmetry-consistent theoretical models of the multiferroic phase.
Main Methods:
- Single-crystal neutron diffraction was performed on Ca2CoSi2O7.
- Measurements were conducted at temperatures ranging from 10 K to 250 K.
Main Results:
- The low-temperature structure at 10 K was refined in the orthorhombic space group P2(1)2(1)2 with a 3 × 3 × 1 supercell.
- Structural parameters were determined and compared with high-temperature data and literature X-ray diffraction results.
- A phase transition from a high-temperature tetragonal structure (P42(1)m) to a low-temperature orthorhombic structure was observed.
Conclusions:
- The precise crystal structure of Ca2CoSi2O7 in its multiferroic phase has been determined.
- The findings provide essential structural information for understanding the magnetoelectric coupling in this material.
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