EPR spectra of V (IV) in zirconolite-rich ceramics

被引:4
作者
Bogomolova, LD [1 ]
Stefanovsky, SV
Troole, AY
Vance, ER
机构
[1] Moscow MV Lomonosov State Univ, Inst Nucl Phys, Moscow 119899, Russia
[2] SIA Radon, Moscow 119121, Russia
[3] Australian Nucl Sci & Technol Org, Menai, NSW 2234, Australia
关键词
D O I
10.1023/A:1004894128436
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
EPR spectra of V4+ in zirconolite-rich ceramics with nominal composition Ca1.00Gd0.01Zr0.99Ti1.99V0.01O7.00 were studied. It was found that these spectra contain the lines of Gd3+ and V4+ ions. Computer calculation of the spectrum of V4+ with hyperfine structure showed that it is a superposition of two spectra of V4+ ions due to V4+ ions substituting for Ti4+ ions in two non-equivalent positions of these ions in zirconolite lattice. The analysis of linewidths of hyperfine components of the V4+ spectrum indicates the correlated positions of Gd and V in the zirconolite lattice with the distance between them r(v)-Gd similar to1 nm. It is assumed that V5+ ions also substitute for Ti4+ ions and compensate the electric charge of Gd3+ ions, which replace Zr4+ in the same unit cell of zirconolite crystal lattice. (C) 2001 Kluwer Academic Publishers.
引用
收藏
页码:1213 / 1217
页数:5
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