Published June 9, 2004
| Version v1
Journal article
Combined wet-chemical process to synthesize 65PMN-35PT nanosized powders
Description
Columbite MgNb2O6 precursors were synthesized by a wet-chemical method by means of the dissolution of Nb2O5.5H2O and magnesium carbonate in a solution of oxalic acid. Pure 65PMN-35PT powders could be obtained by the columbite method with the use of the partial oxalate and oxidant peroxo methods. Powders were characterized by X-ray diffraction and FT-Raman spectroscopy showing that pure 65PMN-35PT are obtained when the powders are calcined up to 800 deg. C, without any trace of Pb-Nb pyrochlore. Cubic Pb1,86Mg0.24Nb1.76O6.5 pyrochlore phase is formed by lead loss in the powders calcined at 900 deg. C and higher temperatures as undoubtedly characterized by Raman spectroscopy
Additional details
Identifiers
- DOI
- 10.1016/j.jallcom.2003.10.013;
- PII
- S0925838803011368;
Publishing Information
- Journal Title
- Journal of Alloys and Compounds
- Journal Volume
- 372
- Journal Issue
- 1-2
- Journal Page Range
- p. 111-115
- ISSN
- 0925-8388
- CODEN
- JALCEU
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 37049296
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- DISSOLUTION; FERROELECTRIC MATERIALS; MAGNESIUM CARBONATES; MAGNESIUM COMPOUNDS; NANOSTRUCTURES; NIOBATES; NIOBIUM OXIDES; OXALATES; OXALIC ACID; OXIDIZERS; PRECURSOR; PYROCHLORE; RAMAN SPECTROSCOPY; SYNTHESIS; TEMPERATURE RANGE 1000-4000 K; X-RAY DIFFRACTION
- Descriptors DEC
- ALKALINE EARTH METAL COMPOUNDS; CARBON COMPOUNDS; CARBONATES; CARBOXYLIC ACID SALTS; CARBOXYLIC ACIDS; CHALCOGENIDES; COHERENT SCATTERING; DICARBOXYLIC ACIDS; DIELECTRIC MATERIALS; DIFFRACTION; LASER SPECTROSCOPY; MAGNESIUM COMPOUNDS; MATERIALS; MINERALS; NIOBIUM COMPOUNDS; ORGANIC ACIDS; ORGANIC COMPOUNDS; OXIDES; OXYGEN COMPOUNDS; REFRACTORY METAL COMPOUNDS; SCATTERING; SPECTROSCOPY; TEMPERATURE RANGE; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2003 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.