Structural stability of the smectite-doped lanthanum under high pressures and high temperatures
Description
Smectites are phyllosilicates that have a tetrahedron: octahedron structure ratio of 2:1, with high cation exchange capacity (CEC) in the interlayers. For these and other features, smectites have been used in many parts of the world as secondary barriers with the goal of containing a possible leak of radioactive elements in final disposal facilities for radioactive waste through cation exchange. Our aim in this work is to reach the cation exchange in calcium montmorillonite (smectite dioctahedral) by lanthanum to simulate trivalent radionuclides and to study the stability of this structure under high pressure and high temperature. To achieve high pressure it was used two different technique: DAC (Diamond Anvil Cell), achieving pressures up to 12GPa at room temperature and hydraulic press with a toroidal chamber profile to achieve pressures up to 7,7GPa and temperatures up to 900 degree C. The heating is achieved simultaneously by an electric system coupled in the hydraulic press. The outcomes show that the smectite structure doped with lanthanum remains stable under 12GPa at room temperature and 2.5GPa at 200 degree C. However, above 300 degree C at 2.5GPa the structure becomes a new phase of muscovite-like, rich of La, where it loses its interlayer water and turns out to be irreversible. Furthermore, it is important to point out that the higher temperature the better ordered is the structure and it is still stable under 7.7GPa and 900 degree C. Moreover, after all experiments the structure continues being dioctahedral. The new phase of muscovite-like, rich of La, in contact with a calcium solution remains partially unchanged, whereas the other part returns to the original structure (montmorillonite-Ca). The following analyses were performed: X-ray diffraction (XRD) for evaluating the spatial structure; Fourier transform infrared spectroscopy (FTIR) for getting information about the vibrational modes; scanning electron microscopy with dispersive Xray spectroscopy (SEM-EDS) to obtain a compositional analysis and transmission electrons microscopy (TEM) to get images with high magnification and high resolution from the samples. (author)
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Additional details
Additional titles
- Original title (Portuguese)
- Estabilidade estrutural da esmectita dopada com lantanio sob altas pressoes e altas temperaturas
Publishing Information
- Imprint Pagination
- 104 p.
- Report number
- INIS-BR--13569
INIS
- Country of Publication
- Brazil
- Country of Input or Organization
- Brazil
- INIS RN
- 44083090
- Subject category
- S36: MATERIALS SCIENCE;
- Resource subtype / Literary indicator
- Thesis
- Descriptors DEI
- CALCIUM; CATIONS; DOPED MATERIALS; FOURIER TRANSFORM SPECTROMETERS; FOURIER TRANSFORMATION; INFRARED SPECTRA; LANTHANUM; MONTMORILLONITE; MUSCOVITE; PRESSURE RANGE MEGA PA 10-100; RADIOACTIVE WASTES; SCANNING ELECTRON MICROSCOPY; SMECTITE; TEMPERATURE RANGE 0400-1000 K; TRANSMISSION ELECTRON MICROSCOPY; X-RAY DIFFRACTION
- Descriptors DEC
- ALKALINE EARTH METALS; CHARGED PARTICLES; CLAYS; COHERENT SCATTERING; DIFFRACTION; ELECTRON MICROSCOPY; ELEMENTS; INORGANIC ION EXCHANGERS; INTEGRAL TRANSFORMATIONS; ION EXCHANGE MATERIALS; IONS; MATERIALS; MEASURING INSTRUMENTS; METALS; MICA; MICROSCOPY; MINERALS; PRESSURE RANGE; PRESSURE RANGE MEGA PA; RADIOACTIVE MATERIALS; RARE EARTHS; SCATTERING; SILICATE MINERALS; SPECTRA; SPECTROMETERS; TEMPERATURE RANGE; TRANSFORMATIONS; WASTES