MÖssbauer Measurements of Interfacial Magnetism of MBE Grown FE(100)/AG(100) Multilayers

1991 ◽  
Vol 231 ◽  
Author(s):  
H. Tang ◽  
M.D. Wieczorek ◽  
D.J. Keavney ◽  
D.F. Storm ◽  
C.J. Gutierrez ◽  
...  

AbstractMultilayers of Fe(100)/Ag(100) were grown by MBE and analyzed with in situ RHEED and MÖssbauer spectroscopy. These films had a constant Ag layer thickness of 40 monolayers (ML) and varying Fe layer thicknesses of 3, 6, and 9 ML. Using MÖssbauer spectroscopy the presence of three Fe sites was inferred. From considerations of the hyperflne parameters and the relative intensities of the sextets, we assign one site to the bulk, and one to each interface: Fe on Ag and Ag on Fe. We believe that one explanation of this is differing tetragonal distortions at the two interfaces. Consequently, another series of films was grown in an attempt to distinguish these sites. These films were essentially identical to the 9 ML film above, but the Fe layers were composed of 56Fe, with a 2 ML 57Fe probe layer effused at the bulk and at each interface in turn. At this point 57Fe MÖssbauer spectroscopy was used to determine the hyperfine field and its temperature dependence for each of the three sites.

2006 ◽  
Vol 167 (1-3) ◽  
pp. 733-738 ◽  
Author(s):  
Abdelmaula Aboulaich ◽  
Florent Robert ◽  
Pierre Emmanuel Lippens ◽  
Laurent Aldon ◽  
Josette Olivier-Fourcade ◽  
...  

Clay Minerals ◽  
1986 ◽  
Vol 21 (2) ◽  
pp. 149-157 ◽  
Author(s):  
S. Bouda ◽  
K. P. Isaac

AbstractBiotites from three peaty gleyed podzol soil profiles on ranite bedrock were examined to investigate the oxidation of the octahedral Fe during weathering. Oxidation of these biotites as determined by Mössbauer spectroscopy shows a good correlation with the in situ measured soil Eh values of the sampled horizons. In every soil profile the highest Eh measured is in the A horizon and the lowest in the C horizon. Similarly, biotites from the A horizons are the most oxidized compared with those from the lower horizons. In most of the samples the oxidation is accompanied by loss of K+ from the lattice, as demonstrated by a moderate degree of vermiculitization.


2003 ◽  
Vol 629 (10) ◽  
pp. 1787-1794 ◽  
Author(s):  
V. Ksenofontov ◽  
S. Reiman ◽  
M. Waldeck ◽  
R. Niewa ◽  
R. Kniep ◽  
...  

2011 ◽  
Vol 207 (1-3) ◽  
pp. 97-105 ◽  
Author(s):  
Iris Fleischer ◽  
◽  
Göstar Klingelhöfer ◽  
Richard V. Morris ◽  
Christian Schröder ◽  
...  

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