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University of Missouri--Rolla

The atomic and magnetic structures of several iron-substituted rare-earth manganese germanides and stannides

Abstract

dc:description.abstract

<p>"NdMn<sub>6-x</sub>Fe<sub>x</sub>Ge<sub>6</sub> , SmMn<sub>6-x</sub>Fe<sub>x</sub>Ge<sub>6</sub> , NdMn<sub>6-x</sub>Fe<sub>x</sub>Sn<sub>6</sub> , and SmMn<sub>6-x</sub>Fe<sub>x</sub>Sn<sub>6</sub> have been studied by x-ray and neutron diffraction techniques and bulk magnetization measurements. NdMn<sub>6-x</sub>Fe<sub>6</sub>Sn<sub>6</sub> has also been studied by Mӧssbauer spectroscopy. All germanides crystallize in the disordered YCo<sub>6</sub>Ge<sub>6</sub>-type structure, whereas the stannides crystallize in the HoFe<sub>6</sub>Sn<sub>6</sub>-type and the TbFe<sub>6</sub>Sn<sub>6</sub>-type structure for the non-substituted samples and the iron-containing samples, respectively. Iron randomly replaces manganese on all sites in both germanides and stannides. The a, b, and c lattice parameters decrease with increasing iron content for all samples. The net magnetization decreases with increasing iron content for all germanides and the stannides with iron content larger than x = 1.24, whereas the net magnetization increases with increasing iron content for the stannides with iron content less than x = 1.24. The magnetic moment of the iron sublattice couples antiferromagnetically with the ferromagnetically coupled manganese and rare-earth moments for the germanides, whereas there is ferromagnetic coupling between the iron sublattice and the ferromagnetically coupled manganese and rare-earth sublattices for the stannides. Spin reorientation occurs in all neodymium- containing samples in which the easy magnetization direction cants away from the c-axis and the a-axis with increasing temperature for the germanides and the stannides, respectively. The easy magnetization direction of all samarium-containing samples is parallel to, or at least aligned at a small angle with, the basal plane of the unit cell at room temperature. An analysis of the Mn-Mn interatomic distances in RMn<sub>6</sub>X<sub>6</sub> and RMn<sub>6</sub>-<sub>x</sub>Fe<sub>x</sub>X<sub>6</sub>, where R is a rare earth and X is germanium or tin, indicates that there is a critical Mn-Mn distance, d<sub>T</sub> ≈ 2.6145 Å, below and above which the coupling within the manganese sublattice is anti ferromagnetic and ferromagnetic, respectively"--Abstract, page iv.</p>

Degree

thesis:*
Name thesis:degree_name
Ph. D. in Chemistry
Grantor
University of Missouri--Rolla
Year dc:date.available
2016

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Han, Jun

Subjects

dc:subject × 1

Identifiers

dc:identifier.*
OAI identifier oai:identifier
oai:scholarsmine.mst.edu:doctoral_dissertations-2366

Chain of custody

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Missouri University of Science and Technology
Base URL
scholarsmine.mst.edu/do/oai/
Last updated
2026-07-24
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citation

Han, Jun. The atomic and magnetic structures of several iron-substituted rare-earth manganese germanides and stannides. University of Missouri--Rolla, 2016. https://scholarsmine.mst.edu/doctoral_dissertations/1364