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Nd3+掺杂钙钛锆石(Ca1-xNdxZrTi2O7+x/2)相变行为的研究OA北大核心CSTPCD

Study on the phase evolution of Nd3+-doped zirconolite ceramics(Ca1-xNdxZrTi2O7+x/2)

中文摘要英文摘要

为研究钙钛锆石对放射性元素Am3+的稳定固化作用,以Nd3+为Am3+的模拟元素,系统研究了高温固相法制备Ca1-xNdxZrTi2O7+x/2时,Nd3+异价取代钙钛锆石晶格中Ca2+位(0≤x≤1.0)所导致的相态演变行为.合成Ca1-x NdxZrTi2O7+x/2的XRD、Raman、BSE和EDS测试结果表明:钙钛锆石(Zirconolite)晶格对Nd3+离子的固溶量可达70%(x=0.7),可有效实现对Am3+模拟元素Nd3+离子的固化.但随着Nd3+掺杂量(x≤0.3)增加,Zirconolite-2M晶格中O2-和Nd3+的无序化程度逐渐增加、(Ca/Nd)-O键长逐渐变小,直至(x=0.4)引起Zr4+、Ti4+附近的O2-配位数发生改变(ZrO7→ZrO8、TiO5→TiO6),Zirconolite-2M晶格结构开始向Zirconolite-4M转变.x=0.5时,陶瓷体完全转变为Zirconolite-4M晶格且O2-和Nd3+有序度重新变高、Ti—O键长增加;直至x=0.6、x=0.7时,陶瓷体仍为单一Zirconolite-4M结构,但晶格中O2-和Nd3+的有序度又逐渐降低,以至于在x=0.7陶瓷体亚晶格中微量Ca2+、Zr4+、Nd3+离子占位转变为烧绿石(Pyrochlore)结构.而在0.8≤x≤0.9范围内,Zirconolite-4M结构完全消失,陶瓷体为多相共存状态(Pyrochlore、ZrTiO4和Nd2(TiZr)4O11物相).Nd3+完全取代Ca2+位(x=1.0)时,陶瓷体变为单一Nd2(TiZr)4O11固溶体相.陶瓷体晶粒的BSE和EDS分析证实了这种相变规律.

This paper used Nd3+ as a surrogate element of Am3+ to simulate the study of the stable curing effect of zirconolite on the radioactive element Am3+.The phase evolution behavior caused by Ca2+ sites in the lattice of Ca1-xNdxZrTi2O7+x/2 with Nd3+ heterovalent substitution was systematically investigated.The Ca1-xNdxZrTi2O7+x/2(0≤x≤1.0)ceramic samples were prepared by high temperature solid-state synthesis and characterized by XRD,Raman,BSE,and EDS analysis.The experimental results showed that the solid solution content of Nd3+ ion could reach up to 70%(viz.x=0.7)in the zirconolite lattice.This indicated that the Nd3+ ion as a substitution element could effectively simulate Am3+ solidification in the zirconolite lattice.However,as the doping amount of Nd3+(x≤0.3)increased,the disordering of the O2-and Nd3+ ions in the zirconolite-2M lattice increased gradually.On the contrary,the(Ca/Nd)-O chemical bond was slightly shortened.Until x=0.4,the O2-coordination number around some Zr4+and Ti4+ ions changed(ZrO7→ZrO8,TiO5→TiO6),partly the zirconolite-2M structure rearrangement to the zirconolite-4M structure.When x=0.5,all the zirconolite-2M structure was converted into zirconolite-4M structure,and the ordering of the O2-and Nd3+ cations increased again,with the Ti-O chemical bond slightly elongated.With increasing x(x=0.6、0.7),the sample still retained a single zirconolite-4M structure,but the ordering of the O2-and Nd3+ cations gradually decreased.When x =0.7,the Ca2+、Zr4+、Nd3+ ions exhibited a subtle amount of pyrochlore structure arrangement in the sublattice.When 0.8≤x≤0.9,the samples converted to a polyphase coexistence state(Pyrochlore,ZrTiO4 and Nd2(TiZr)4O11).Finally,a single Nd2(TiZr)4O11 solid solution phase was observed when x = 1.0.Further,the composition and microstructure of coexisting phases were verified by BSE and EDS.

提学超;李伟民

四川航天职业技术学院飞行器制造学院,四川 广汉 618300西南科技大学国防科技学院,四川 绵阳 621000

核科学

Nd3+-掺杂钙钛锆石-2M相关系有序-无序

Nd3+-dopedzirconolite-2Mphase relationshipordering-disordering

《有色金属科学与工程》 2024 (002)

302-310 / 9

国家863"高放废液分离、处理工艺及关键设备技术研究资助项目"(2009AA050703)

10.13264/j.cnki.ysjskx.2024.02.017

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