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Effect of temperature on formation of murataite and murataite-pyrochlore ceramics

机译:温度对钙钛矿和钙钛矿-烧绿石陶瓷形成的影响

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Processes of phases formation in the ceramic mixtures with basic compositions (wt.%) 10 CaO, 10 MnO, 5 Al_2O_3,5 Fe_2O_3, 55 TiO_2, 5 ZrO_2,10 UO_2 (M1) and 8 CaO, 8 MnO, 4 Al_2O_3, 4 Fe_2O_3, 20 Gd_2O_3, 44 TiO_2, 4 ZrO_2, 8 UO_2 (M4) were studied using X-ray diffraction, scanning and transmission electron microscopy. The batches were milled, compacted in pellets at 200 MPa, and heat-treated in a resistive furnace at 1100℃, 1300℃, 1400℃, and 1500℃ as well as melted in a cold crucible at ~1600 ℃. Reactions in the mixtures heat-treated at 1100 C were not completed and samples contained significant amount of unreacted and intermediate (altered rutile, cubic oxide solid solution, perovskite) phases. Within the temperature range 1100-1300℃ reactions are mainly completed and ceramics sintered at 1300℃ are composed of major murataite and minor rutile (M1) or major murataite and pyrochlore and minor zirconolite and perovskite (M4). However full homogenization at 1300℃ has not been reached yet and to obtain the ceramics with uniform compositions of the phases sintering at 1400℃ or melting at 1500-1600℃ were required. In the ceramic sample Ml two murataite varieties with five- (murataite-5C) and eight-fold (mu-rataite-8C) fluorite-type unit cells were found. The sample M4 is composed of pyrochlore, murataite-8C and zircqnolite-3O. In the sample Ml murataite-5C is enriched with U and Ca and depleted with iron group elements as compared to murataite-8C. Fraction of murataite-5C concentrates about 80% of total U and about 70% of Mn+Fe (corrosion products). Waste elements partitioning among the phases in the M4 sample depends significantly on temperature of heat-treatment.
机译:基本成分(wt。%)10 CaO,10 MnO,5 Al_2O_3、5 Fe_2O_3、55 TiO_2、5 ZrO_2、10 UO_2(M1)和8 CaO,8 MnO,4 Al_2O_3、4的陶瓷混合物中的相形成过程用X射线衍射,扫描和透射电镜研究了Fe_2O_3、20 Gd_2O_3、44 TiO_2、4 ZrO_2、8 UO_2(M4)。将批料研磨,在200 MPa下压成颗粒,并在1100℃,1300℃,1400℃和1500℃的电阻炉中进行热处理,并在〜1600℃的冷坩埚中熔化。在1100℃下热处理的混合物中的反应未完成,并且样品含有大量未反应的和中间的(改变的金红石,立方氧化物固溶体,钙钛矿)相。在1100-1300℃的温度范围内,反应基本完成,在1300℃下烧结的陶瓷由主要的褐铁矿和次要金红石(M1)或主要的褐铁矿和烧绿石以及次要的锆石和钙钛矿(M4)组成。然而,尚未达到在1300℃下的完全均质化,并且需要获得具有在1400℃下烧结或在1500-1600℃下熔融的相组成均匀的陶瓷。在陶瓷样品M1中,发现了具有五种(murataite-5C)和八倍的(mu-rataite-8C)萤石类型的晶石型晶石。样品M4由烧绿石,Murataite-8C和Zrqqnolite-3O组成。在样品M1中,与murataite-8C相比,murataite-5C富含U和Ca,并且贫有铁族元素。 murataite-5C的馏分集中了约80%的总U和约70%的Mn + Fe(腐蚀产物)。在M4样品的各相之间分配的废物元素在很大程度上取决于热处理温度。

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