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Cementite Orthorhombic Crystal Structure

The cementite phase of Fe 3 C has been studied by highresolution neutron powder diffraction at 4.2 K and at 20 K intervals between 20 and 600 K. The crystal structure remains orthorhombic Pnma throughout, with the fractional coordinates of all atoms varying only slightly the magnetic structure of the ferromagnetic phase could not be determined.

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