Effects of calcination on microscopic and mesoscopic structures in Ca- and Sr-doped nano-crystalline lanthanum chromites
Creators
- 1. High Pressure and Synchrotron Radiation Physics Division, Bhabha Atomic Research Centre, Trombay, Mumbai 400085 (India)
- 2. Solid State Physics Division, Bhabha Atomic Research Centre, Trombay, Mumbai 400085 (India)
- 3. Materials Processing Division, Bhabha Atomic Research Centre, Trombay, Mumbai 400085 (India)
Description
Calcination behavior of nano-crystalline lanthanum chromites doped with calcium and strontium has been probed by Fourier transform infrared spectroscopy, X-ray diffraction and small-angle neutron scattering as a function of temperature. Infrared spectroscopic results imply that over a range of temperatures, some intermediate phase of dopant chromates evolve and then dissolve back, which has also been confirmed by the XRD. Neutron scattering data reveal a fractal type correlation of building blocks in virgin powders. Increase in fractal dimension and reduction in upper cutoff vis-a-vis the densification of agglomerates were found with increasing calcination temperature. Calcination, beyond 900 oC, results in breaking down of the fractal morphology almost completely. Such shrinkage event also results in a modification of the microscopic structure. These changes have been attributed to the compaction of agglomerates of both Ca- and Sr-doped lanthanum chromites, assisted via liquid state sintering by the melting of the intermediate phases at intermediate calcination stages. -- Graphical Abstract: Dopant chromates evolve as intermediate phases during calcination of Ca- and Sr-doped nano-crystalline lanthanum chromites at intermediate temperatures, around 900 oC, evident from infrared spectroscopy. Such an event results in a modification of the microscopic and mesoscopic structures. Display Omitted Research highlights: → Meso/microscopic structures of La0.7Ca0.3CrO3 and La0.8Sr0.2CrO3 modify during calcination. → Transient phases CaCrO4 and SrCrO4 appear at intermediate temperatures. → Bond length, unit cell volume, etc. modify as intermediate phases evolve and extinct. → Compaction of the agglomerates takes place due to liquid state assisted sintering.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.jssc.2010.11.006Additional details
Identifiers
- DOI
- 10.1016/j.jssc.2010.11.006;
- PII
- S0022-4596(10)00512-8;
Publishing Information
- Journal Title
- Journal of Solid State Chemistry
- Journal Volume
- 184
- Journal Issue
- 1
- Journal Page Range
- p. 204-213
- ISSN
- 0022-4596
- CODEN
- JSSCBI
INIS
- Country of Publication
- United States
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 42085994
- Subject category
- S36: MATERIALS SCIENCE; S77: NANOSCIENCE AND NANOTECHNOLOGY;
- Descriptors DEI
- ABSORPTION SPECTROSCOPY; BOND LENGTHS; CALCINATION; CHROMATES; CHROMIUM OXIDES; DOPED MATERIALS; FRACTALS; INFRARED SPECTRA; LANTHANUM OXIDES; MELTING; MORPHOLOGY; NANOSTRUCTURES; NEUTRON DIFFRACTION; PEROVSKITE; SINTERING; SMALL ANGLE SCATTERING; SOLID OXIDE FUEL CELLS; STRONTIUM; TEMPERATURE DEPENDENCE; TEMPERATURE RANGE 1000-4000 K; X-RAY DIFFRACTION
- Descriptors DEC
- ALKALINE EARTH METALS; CHALCOGENIDES; CHEMICAL REACTIONS; CHROMIUM COMPOUNDS; COHERENT SCATTERING; DECOMPOSITION; DIFFRACTION; DIMENSIONS; DIRECT ENERGY CONVERTERS; ELECTROCHEMICAL CELLS; ELEMENTS; FABRICATION; FUEL CELLS; HIGH-TEMPERATURE FUEL CELLS; LANTHANUM COMPOUNDS; LENGTH; MATERIALS; METALS; MINERALS; OXIDE MINERALS; OXIDES; OXYGEN COMPOUNDS; PEROVSKITES; PHASE TRANSFORMATIONS; PYROLYSIS; RARE EARTH COMPOUNDS; SCATTERING; SOLID ELECTROLYTE FUEL CELLS; SPECTRA; SPECTROSCOPY; TEMPERATURE RANGE; THERMOCHEMICAL PROCESSES; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2010 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.