Adamska, A. M. ; Havela, L. ; Danis, S. ; Pesicka, J. ; Macl, J. ; Uhlirova, K. ; Gouder, T. ; Eloirdi, R. ; Huber, F. ; Kim-Ngan, N.-T. H. ; Balogh, A. G. (2010)
Uranium compounds prepared by sputter deposition: UFe2+x.
In: Journal of Physics: Conference Series, 200 (1)
Article
Abstract
UFe2 is one of rare examples of combination of 3d and 5f magnetism in a compound with relatively high TC = 162 K. U-excess is known to reduce the TC value markedly. To prepare the Laves phase with an Fe excess is much more difficult. It can be achieved by sputter deposition, but the structure becomes amorphous. TC can increase at least to 240 K (for UFe4), but the segregation of α-Fe cannot be avoided for very high Fe concentrations.
Item Type: | Article |
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Erschienen: | 2010 |
Creators: | Adamska, A. M. ; Havela, L. ; Danis, S. ; Pesicka, J. ; Macl, J. ; Uhlirova, K. ; Gouder, T. ; Eloirdi, R. ; Huber, F. ; Kim-Ngan, N.-T. H. ; Balogh, A. G. |
Type of entry: | Bibliographie |
Title: | Uranium compounds prepared by sputter deposition: UFe2+x |
Language: | English |
Date: | 2010 |
Publisher: | IOP Publishing |
Journal or Publication Title: | Journal of Physics: Conference Series |
Volume of the journal: | 200 |
Issue Number: | 1 |
URL / URN: | http://iopscience.iop.org/1742-6596/200/1/012057/ |
Abstract: | UFe2 is one of rare examples of combination of 3d and 5f magnetism in a compound with relatively high TC = 162 K. U-excess is known to reduce the TC value markedly. To prepare the Laves phase with an Fe excess is much more difficult. It can be achieved by sputter deposition, but the structure becomes amorphous. TC can increase at least to 240 K (for UFe4), but the segregation of α-Fe cannot be avoided for very high Fe concentrations. |
Uncontrolled Keywords: | Condensed matter: electrical, magnetic and optical Surfaces, interfaces and thin films |
Divisions: | 11 Department of Materials and Earth Sciences > Material Science > Material Analytics 11 Department of Materials and Earth Sciences > Material Science 11 Department of Materials and Earth Sciences |
Date Deposited: | 06 Dec 2010 12:48 |
Last Modified: | 31 Oct 2016 10:05 |
PPN: | |
Funders: | This work was supported by the Grant Agency of the Academy of Sciences of the Czech Republic under the grant number IAA100100912 and by the Czech Research and Development project KAN101630651., N.-T.H.K-N and A.G.B. acknowledge the financial support from German Academic Exchange Service (DAAD)-project D/08/07991. |
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