scholarly journals XRD and TEM analyses of a simulated leached rare earth ore deposit: Implications for clay mineral contents and structural evolution

2021 ◽  
Vol 225 ◽  
pp. 112728
Author(s):  
Xiongwei Jin ◽  
Lingkang Chen ◽  
Haixia Chen ◽  
Lian Zhang ◽  
Wenjing Wang ◽  
...  
2019 ◽  
Vol 237 ◽  
pp. 121830 ◽  
Author(s):  
S.E. Kichanov ◽  
Yu.E. Gorshkova ◽  
G.E. Rachkovskaya ◽  
D.P. Kozlenko ◽  
G.B. Zakharevich ◽  
...  

2006 ◽  
Vol 20 (25n27) ◽  
pp. 4010-4015 ◽  
Author(s):  
XIAOJUAN JI ◽  
QIULI WEI ◽  
CHUNGEN ZHOU ◽  
SHENGKAI GONG ◽  
HUIBIN XU

Decreasing thermal diffusivity of YSZ can increase the thermal barrier effect. Thermal diffusivity is in direct proportion to lattice oscillation amplitude and frequency. The addition of rare earth oxide into YSZ may induce the lattice distortion, which will result in the change of lattice oscillation frequency. In the present work, combined with the experiment, a theoretical study was proposed to investigate the effect of the rare earth elements on the thermal barrier effect of YSZ using first-principal calculations implemented CASTEP program. It has been found that the addition of the rear earth element can make larger lattice distortion and favorable to reduce the thermal conductivity. The calculation results are in agreement with our experimental results.


2020 ◽  
Vol 33 (3) ◽  
pp. 035405
Author(s):  
Wang Yongyong ◽  
Zhang Panpan ◽  
Li Qing ◽  
Li Gong

2019 ◽  
Vol 2019 ◽  
pp. 1-10 ◽  
Author(s):  
Luca Spiridigliozzi ◽  
Grazia Accardo ◽  
Domenico Frattini ◽  
Antonello Marocco ◽  
Serena Esposito ◽  
...  

In this work, nanoparticles of cerium hydroxycarbonates were synthesized by a facile hydrothermal treatment at 120°C with ammonium carbonate as the precipitating/mineralizer agent in diluted solution. The as-formed amorphous coprecipitate undergoes several morphological and structural modifications as a function of the duration of the hydrothermal treatment, leading after 8 h to the formation of monosized nanoparticles of hexagonal CeCO3OH. A similar behavior has been found when neodymium-based precursors are used as well, whereas the same treatment produces very different results by using different lanthanides-based precursors in terms of formed phases and morphologies, thus leading to the formation of pure tengerite-type structure phases, biphasic systems (tengerite type and hexagonal), or even entirely amorphous systems. Furthermore, the hydrothermal transformation is influenced by the redox behavior of the rare-earth cation (i.e., cerium) too, eventually resulting in the formation of fluorite-like structures. Therefore, a specific pathway of Ce(III) precursor transformations during hydrothermal treatment is proposed in this paper. Definitely, our results show that ammonium carbonate can be used as the precipitating/mineralizer agent to obtain cerium, doped-cerium, and neodymium hydroxycarbonates, which show excellent morphologies (i.e., characterized by spherical, nanosized particles with monomodal size distribution). Therefore, they can be used as optimal precursors for oxide powders. Conversely, when tengerite-type carbonate precursors are formed, their morphology is characterized by large and acicular particles.


1991 ◽  
Vol 257 ◽  
Author(s):  
E.R. Vance ◽  
K.L. Smith ◽  
G.J. Thorogood ◽  
B.D. Begg ◽  
S.S. Moricca ◽  
...  

ABSTRACTPerovskite is the least durable of the resistate minerals comprising Synroc-C and it is desirable to reduce its abundance in Synroc. Kinetic limitations and competition with Csapparently affect the incorporation of Sr into hollandite during hot-pressing at 1200ºC/20 MPa so that ∼ 10% of perovskite (a value below the percolation limit) is probably an optimum target. Zirconolite-rich Synroc formulations have been prepared for actinide-rich wastes. Background XRD and TEM studies have also been performed to study the crystal-chemical behaviour of Nd (a simulant of trivalent actinides) in zirconolite. Either rare-earth compensated perovskite or freudenbergite in Synroc can evidently be used to immobilise Na-bearing HLW.


1990 ◽  
Author(s):  
E.C. Chao ◽  
Mitsunobu Tatsumoto ◽  
R.L. Erickson ◽  
J.A. Minkin ◽  
J.M. Back ◽  
...  

Clay Minerals ◽  
1998 ◽  
Vol 33 (3) ◽  
pp. 483-500 ◽  
Author(s):  
M. Ortega ◽  
I. Palomo ◽  
F. Martinez ◽  
I. Gonzalez

AbstractThe clay mineral associations in the Cretaceous-Tertiary Boundary (KTB) and in the Danian and Maastrichtian levels of sections from the Mediterranean and the Atlantic Domains have been studied. The Mediterranean sections have a single mineral association consisting of smectiteiltite and kaolinite, whereas the Atlantic sections have several associations: illite-chlorite, illite-R1 I-S-kaolinite and illite-R 1 I-S-chlorite. Data are presented relating to the influence of K-feldspars and Fe oxide sphemles on the clay mineral associations. Study of rare-earth elements shows that regional geological factors affect the clay mineralogy of the KTB, examples showing significant anthigenesis in the Mediterranean sections, and important detrital supply in all the Atlantic sections. We propose that the KTB studied in these marine sections is equivalent to the uppermost layer of the two-layered clay unit originating in a cloud of a vapourized bolide. Regional tectonic conditions have been responsible for differences in clay sedimentation in these geological domains and among the stratigraphic sections of the Atlantic Domain.


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