TY - JOUR
T1 - Oxygen stoichiometry in the (Ba0.5La0.5) (Fe1-xCux)O3-w (x=0-1) perovskite system
AU - Lehmus, K.
AU - Karppinen, M.
AU - Matvejeff, M.
AU - Lindén, J.
AU - Pietari, T.
AU - Yamauchi, H.
PY - 2001
Y1 - 2001
N2 - Oxygen stoichiometry in the perovskite system (Ba0.5La0.5) (Fe1-xCux)O3-w with x varying in the range of 0 to 1 was studied by thermogravimetry, 57Fe Mössbauer spectroscopy and different wet-chemical analysis methods. Both the maximum oxygen content and the amount of removable oxygen strongly depended on the copper-to-iron ratio. In this respect the samples containing both copper and iron were nearly identical but differed from the end members of the system. In the samples with 0.1≤x≤0.85 the maximum oxygen content varied in the narrow range of w = 0.25-0.33 whereas for the x = 0 and x = 1 samples the values of w = 0.06 and 0.60, respectively, were determined. The amount of removable oxygen (Δw) was the smallest for the Fe-free sample. It is interesting to note that, the maximum oxygen content of the x = 0.5 sample (as well as the samples with 0.15≤x≤0.85) was found to continue the trend of decreasing w with increasing RE ion size, as previously observed for the double-perovskite series BaRE(Fe0.5Cu0.5)2O5+8.
AB - Oxygen stoichiometry in the perovskite system (Ba0.5La0.5) (Fe1-xCux)O3-w with x varying in the range of 0 to 1 was studied by thermogravimetry, 57Fe Mössbauer spectroscopy and different wet-chemical analysis methods. Both the maximum oxygen content and the amount of removable oxygen strongly depended on the copper-to-iron ratio. In this respect the samples containing both copper and iron were nearly identical but differed from the end members of the system. In the samples with 0.1≤x≤0.85 the maximum oxygen content varied in the narrow range of w = 0.25-0.33 whereas for the x = 0 and x = 1 samples the values of w = 0.06 and 0.60, respectively, were determined. The amount of removable oxygen (Δw) was the smallest for the Fe-free sample. It is interesting to note that, the maximum oxygen content of the x = 0.5 sample (as well as the samples with 0.15≤x≤0.85) was found to continue the trend of decreasing w with increasing RE ion size, as previously observed for the double-perovskite series BaRE(Fe0.5Cu0.5)2O5+8.
KW - Mössbauer spectroscopy
KW - Oxides
KW - Thermogravimetric analysis
KW - X-ray diffraction
UR - http://www.scopus.com/inward/record.url?scp=0035652336&partnerID=8YFLogxK
U2 - 10.1016/S1466-6049(01)00177-5
DO - 10.1016/S1466-6049(01)00177-5
M3 - Article
AN - SCOPUS:0035652336
SN - 1466-6049
VL - 3
SP - 803
EP - 808
JO - International Journal of Inorganic Materials
JF - International Journal of Inorganic Materials
IS - 7
ER -