首页> 外文会议>International Conference on Radioactive Waste Management and Environmental Remediation >CRYSTALLIZATION SEQUENCE AND MICROSTRUCTURE EVOLUTION OF SYNROC SAMPLES CRYSTALLIZED FROM CaZrTi{sub}2O{sub}7 AND CaCeTi{sub}2O{sub}7 SYSTEMS: HRTEM/AEM INVESTIGATION
【24h】

CRYSTALLIZATION SEQUENCE AND MICROSTRUCTURE EVOLUTION OF SYNROC SAMPLES CRYSTALLIZED FROM CaZrTi{sub}2O{sub}7 AND CaCeTi{sub}2O{sub}7 SYSTEMS: HRTEM/AEM INVESTIGATION

机译:Synroc样品的结晶序列和微观结构演进从Cazrti {sub} 2o {sub} 7和caceti {sub} 2o {sub} 7系统:HRTEM / AEM调查

获取原文

摘要

Scanning electron microscopy (SEM), high-resolution transmission electron microscopy (HRTEM), and analytical electron microscopy (AEM) studies have been conducted on samples crystallized from melts with a composition of zirconolite {(Ca{sub}0.9Gd{sub}0.1)Zr(Ti{sub}1.9Al{sub}0.1){sub}2O{sub}7 and CaCeTi{sub}2O{sub}7. The formation of a whole suite of Synroc phases (zirconia, ZrTiO{sub}4, zirconolite, perovskite, and rutile) has been observed. In the CaZrTi{sub}2O{sub}7 system, the formation of these minerals follows the crystallization sequence of Ti-bearing zirconia → ZrTiO{sub}4 phase → Zr-rich zirconolite → Zrpoor zirconolite → rutile/perovskite. This sequence is induced by a fractional crystallization process, in which Zrrich mineral phases tend to crystallize first, resulting in continuous depletion of Zr in melt. Consistent with this melt compositional evolution, the Zr content in the zirconolite decreases from the area next to the ZrTiO{sub}4 phase to areas next to rutile or perovskite. High-resolution TEM images show that there are no glassy phases at the grain boundary between zirconolite and perovskite. The fractional crystallization-induced textural heterogeneity may have a significant impact on the incorporation of radionuclides into crystalline phases and the resistance of radionuclides to leaching processes. Exsolution lamellae and multiple twinning resulting from the phase transition from tetragonal zirconia to monoclinic zirconia may decrease durability of the Synroc. Fast cooling of the melt may produce more zirconolite phase and relatively uniform texture. In the CaCeTi{sub}2O{sub}7 system, the formation of these minerals follows the crystallization sequence of CeO{sub}2 → Ce-rich pyrochlore → Ce-poor pyrochlore → perovskite. In general, however, a Synroc prepared by melting is less uniform in texture than that prepared by a sol-gel method.
机译:扫描电子显微镜(SEM),高分辨率透射电子显微镜(HRTEM)和分析电子显微镜(AEM)研究已经在用氧化锆组合物结晶的样品上进行了研究(CA {} 0.9gd {} 0.1 )zr(ti {sub} 1.9al {sub} 0.1){sub} 2o {sub} 7和caceti {sub} 2o {sub} 7。已经观察到形成整体Synroc阶段(氧化锆,ZrTiO {Sub} 4,锆石,钙钛矿和金红石)。在Cazrti {sub} 2o {sub} 7系统中,这些矿物的形成遵循Ti轴承氧化锆的结晶序列→Zrtio {sub} 4相→Zr-富锆锆→Zrpoor Zironolite→金润/钙钛矿。该序列由分数结晶过程引起的,其中Zrrich矿物相能首先结晶,导致熔体中的Zr连续耗尽。含有该熔体组成的演化一致,锆醇中的Zr含量从ZrTiO {Sub} 4相旁边的区域降低到金红石或钙钛矿旁边的区域。高分辨率TEM图像表明,锆龙与钙钛矿之间的晶界中没有玻璃阶段。分数结晶诱导的纹理异质性可能对放射性核素掺入结晶相和放射性核素的抗性掺入浸出方法的显着影响。由四边形氧化锆与单斜氧化锆的相转变产生的eX浮出水薄片和多个孪晶可能降低Synroc的耐久性。熔体的快速冷却可以产生更多的锆石相和相对均匀的质地。在CaCeTi {子} 2O {子} 7系统中,这些矿物的形成如下的CeO {子}的结晶序列2→富含Ce的烧绿石→烧绿石的Ce-差→钙钛矿。然而,通常,通过熔化制备的Synroc在质地上的均匀性比通过溶胶 - 凝胶法制备的纹理均匀。

著录项

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号