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 × 1Identifiers
dc:identifier.*- Repository record dc:identifier
- https://scholarsmine.mst.edu/doctoral_dissertations/1364
- OAI identifier oai:identifier
- oai:scholarsmine.mst.edu:doctoral_dissertations-2366