Nuclear inelastic scattering studies of lattice dynamics in magnetite with a first- and second-order Verwey transition

被引:17
作者
Kolodziej, Tomasz [1 ]
Kozlowski, Andrzej [1 ]
Piekarz, Przemyslaw [2 ]
Tabis, Wojciech [1 ]
Kakol, Zbigniew [1 ]
Zajac, Marcin [3 ]
Tarnawski, Zbigniew [1 ]
Honig, Juergen M. [4 ]
Oles, Andrzej M. [5 ]
Parlinski, Krzysztof [2 ]
机构
[1] AGH Univ Sci & Technol, Fac Phys & Appl Comp Sci, PL-30059 Krakow, Poland
[2] Polish Acad Sci, Inst Nucl Phys, PL-31342 Krakow, Poland
[3] European Synchrotron Radiat Facil, F-38043 Grenoble, France
[4] Purdue Univ, Dept Chem, W Lafayette, IN 47907 USA
[5] Jagiellonian Univ, M Smoluchowski Inst Phys, PL-30059 Krakow, Poland
来源
PHYSICAL REVIEW B | 2012年 / 85卷 / 10期
关键词
AUGMENTED-WAVE METHOD; DENSITY-OF-STATES; HEAT-CAPACITY; SYNCHROTRON-RADIATION; RESONANT SCATTERING; NEUTRON-SCATTERING; SINGLE-CRYSTAL; FE3O4; STOICHIOMETRY; ABSORPTION;
D O I
10.1103/PhysRevB.85.104301
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Nuclear inelastic-scattering studies were performed to infer temperature evolution of iron atom dynamics in magnetite samples exhibiting Verwey transition of first-and second-order (type-I and type-II materials). The possible difference in this evolution could rationalize the distinct properties of these classes of materials observed in heat capacity and diffuse scattering below the Verwey transition temperature T-V and could explain the change in transition order triggered by a minute (below 0.3%) altering of the iron sublattice. Although we have found the apparent stiffening of the phonon iron spectrum in the low-temperature phase, at the same time, we have shown that these spectra are rather similar for type-I and type-II materials, rendering the lattice vibration-based explanation of the distinct behavior of heat capacities very improbable. The calculation of phonon spectra, aimed at tracing the origin of various features in the phonon density of states (DOS), has shown that the local Coulomb interaction U may have a large effect on phonon DOS. However, the change in the U parameter cannot explain the difference in heat-capacity results for both classes of materials. Thus, an additional factor that differentiates these materials and possibly is responsible for the discontinuous character of the Verwey transition in stoichiometric magnetite still must be found.
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页数:10
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