On the Crystal Chemistry and Stability of Sm2+ in SmSO4 and Solid Solutions of M1−xSmxSO4 (M=Ba, Sr)
Solid solution formation of Sm2+ and MSO4 (M=Sr, Ba) was investigated for syntheses using (i) a LiCl high-temperature solution exposed to a reducing atmosphere and (ii) precipitation reactions at room temperature starting from aqueous solutions of SmI2 or electrochemically gained Sm2+. In contrast t...
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Published in: | Journal of solid state chemistry Vol. 154; no. 2; pp. 535 - 541 |
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Main Authors: | , , , , , |
Format: | Journal Article |
Language: | English |
Published: |
San Diego, CA
Elsevier Inc
01-11-2000
Elsevier |
Subjects: | |
Online Access: | Get full text |
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Summary: | Solid solution formation of Sm2+ and MSO4 (M=Sr, Ba) was investigated for syntheses using (i) a LiCl high-temperature solution exposed to a reducing atmosphere and (ii) precipitation reactions at room temperature starting from aqueous solutions of SmI2 or electrochemically gained Sm2+. In contrast to (ii), present results show that a high-temperature approach (i) yielded only a very low amount of Sm2+ in M1−xSmxSO4. Formation of a solid solution system (0<x<1) was confirmed for Sr1−xSmxSO4 and Ba1−xSmxSO4 by X-ray powder diffraction analysis and optical lifetime measurements. The unit cell parameters of Ba1−xSmxSO4 showed a slight deviation from Vegard's law. Positive and negative deviations are in agreement with results on solid solutions of Ba1−xSrxSO4. Compounds obtained by syntheses at room temperature were exposed to annealing at 450 to 850°C using a reducing or oxidizing atmosphere. In this temperature range, M1−xSmxSO4 (M=Sr, Ba) decomposed into Sm2O2(SO4) and the corresponding MSO4. Solid solutions of M1−xSmxSO4 (M=Ba, Sr) represent a new system for investigating Sm2+ in an oxide environment. There are only a few other oxide host lattices stabilizing divalent samarium. |
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Bibliography: | ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 |
ISSN: | 0022-4596 1095-726X |
DOI: | 10.1006/jssc.2000.8876 |