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The objective of this work is to synthesize mullite from associated rare-earth kaolin. The effects of 300 mesh (48 μm) and 400 mesh (38 μm) associated rare earth kaolin and sintering temperature on the phase composition, microstructure, sintering behavior, and mechanical properties of mullite were studied. The study showed that the relative mullite content, average aspect ratio, relative density, micro Vickers hardness, and flexural strength of mullite synthesized by using 400-mesh calcined associated rare earth kaolin as raw material and sintered at 1500°C for 4 h were 76.6%, 5.55 μm, 90.19%, 12.05 GPa, and 166.35 MPa, respectively. Compared with mullite synthesized from 300-mesh calcined associated rare earth kaolin, the use of 400-mesh associated rare earth kaolin can reduce the mullitization temperature by about 100°C, increase the average aspect ratio and relative density of mullite by 5.23% and 9.47%, and increase the microscopic Vickers hardness and flexural strength by 6.09% and 17.04%, respectively. This provides new ideas for the comprehensive utilization of associated rare earth kaolin mineral resources and new ways for the high value-added utilization of associated rare earth kaolin, which has great economic value. [ABSTRACT FROM AUTHOR]

The aim of this work is to prepare interlocking prismatic mullite from low‐cost associated rare‐earth kaolin. High‐performance mullite was synthesized by reaction sintering using calcined associated rare‐earth kaolin and α‐Al2O3 as raw materials and micro‐ and nano‐La2O3 as additives. The mineralogical, morphological, and chemical characteristics of calcined associated rare earth kaolin were analyzed, and the effects of the addition of micro‐ and nano‐La2O3 and sintering temperature on the phase transformation, sintering process, microstructure, and mechanical properties of mullite were studied. The results show that the associated rare earth elements Ce, Th, and Y in calcined kaolin are mainly light rare earth elements, which are mainly endowed in the interlayer structure of K‐bearing clay minerals. The addition of La2O3 can promote the growth of secondary mullite grains and accelerate the secondary mullitization process. The relative densities of mullite samples adding 4 wt.% micro/nano La2O3 and sintered at 1500°C for 4 h were 92.72% and 93.4%, and the micro Vickers hardnesses were 11.32 and 12.35 GPa, respectively. The mullite sample with 2 wt.% nano‐La2O3 had the most interlaced prismatic grains, resulting in the highest flexural strength of 157.8 MPa. [ABSTRACT FROM AUTHOR]

The objective of this work was to prepare high‐purity, high‐strength mullite ceramics from low‐cost, associated rare‐earth kaolin (AREK). A reaction sintering process using calcined AREK and γ‐Al2O3 powders was used to synthesize high‐performance mullite ceramics. Mineralogical, morphological, and chemical characteristics of AREK were given. The effects of associated REEs in kaolin and sintering temperature on the microstructural evolution, phase transformation, and physical properties of mullite were studied. The results showed that the mullite contents were 98.8%, the maximum aspect ratio was 8.22 μm, the relative density was 93.04%, and the micro‐Vickers hardness and flexural strength were 10.63 GPa and 184.24 MPa, after sintering at 1500°C for 4 h. For comparison, calcined without rare‐earth kaolin was also employed as a raw material to synthesize mullite ceramics, and the mullite content prepared by sintering the two kaolin clays at 1320–1480°C for 4 h was quite similar. However, mullite prepared using AREK forms secondary mullite in the temperature range of 1480–1500°C with a significantly higher mullite content, and therefore, the advantages of preparing mullite based on AREK as the raw material are high purity, low mullitization temperature, and high strength. [ABSTRACT FROM AUTHOR]

The article present a study on the rare earth elements (REE)-rich clay rocks at the top of the Emeishan basalt in the eastern Yunnan-Western Guizhou area, China. It further discusses REE metallogenic conditions and element occurrence states, and the genetic mechanism; petrographic section measurement, thin section identification and X-ray diffraction analysis; and REE-rich clay rock layered with horizontal bedding and block bedding.