In situ structural changes during toluene complete oxidation on supported EuCoO3 monitored with 151Eu Mössbauer spectroscopy

2006 ◽  
Vol 117 (1-3) ◽  
pp. 329-336 ◽  
Author(s):  
M ALIFANTI ◽  
M FLOREA ◽  
G FILOTTI ◽  
V KUNCSER ◽  
V CORTESCORBERAN ◽  
...  
Keyword(s):  
Mössbauer Spectroscopy ◽  
Structural Changes ◽  
Mossbauer Spectroscopy ◽  
Complete Oxidation ◽  
Mößbauer Spectroscopy ◽  
151Eu Mössbauer Spectroscopy

In situ 119Sn Mössbauer spectroscopy study of Sn-based electrode materials

2006 ◽  
Vol 167 (1-3) ◽  
pp. 733-738 ◽  
Author(s):  
Abdelmaula Aboulaich ◽  
Florent Robert ◽  
Pierre Emmanuel Lippens ◽  
Laurent Aldon ◽  
Josette Olivier-Fourcade ◽  
...  
Keyword(s):  
Mössbauer Spectroscopy ◽  
Electrode Materials ◽  
Mossbauer Spectroscopy ◽  
Spectroscopy Study ◽  
119Sn Mössbauer Spectroscopy ◽  
Mößbauer Spectroscopy

151Eu Mössbauer spectroscopy of the filled skutterdite-type compound EuRu4P12

2002 ◽  
pp. 143-146
Author(s):  
Kentaro Indoh ◽  
Hideya Onodera ◽  
Chihiro Sekine ◽  
Ichimin Shirotani ◽  
Yasuo Yamaguchi
Keyword(s):  
Mössbauer Spectroscopy ◽  
Mossbauer Spectroscopy ◽  
Mößbauer Spectroscopy ◽  
Type Compound ◽  
151Eu Mössbauer Spectroscopy

Influence of soil redox conditions on oxidation of biotite

Clay Minerals ◽  
1986 ◽  
Vol 21 (2) ◽  
pp. 149-157 ◽  
Author(s):  
S. Bouda ◽  
K. P. Isaac
Keyword(s):  
Mössbauer Spectroscopy ◽  
Soil Profile ◽  
Mossbauer Spectroscopy ◽  
Redox Conditions ◽  
Soil Profiles ◽  
Moderate Degree ◽  
Soil Redox ◽  
Mößbauer Spectroscopy

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.

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