摘要
本文定义了稀土元素与其它元素之间的加权平均电负性差P和加权平均原子赝势半径差Q。发现具有较好磁性能的稀土永磁材料的P ,Q值点基本上分布在一个特定的狭带区范围内 ,而高Tc氧化物超导体的P ,Q值点基本上也分布在另一个特定的区域范围内 ,而且这两个区域的走向基本平行。
The weighted average differences P of electronegativ ities and Q of a tomic pseudoradii are defined and calculated. The P,Q value points of the rare e arth permanent magnet materials with good magnetic properties are almost distrib uted into a specific narrow ranges, meanwhile the P,Q value points of the oxide high Tc superconductors are almost distributed into another specific rang es , and the directions of the two ranges are nearly parallel. The result is use ful for investigating new high Tc superconductors.
出处
《闽江学院学报》
2002年第6期47-49,共3页
Journal of Minjiang University
基金
国家 8 6 3计划资助项目
关键词
氧化物超导体
稀土元素
永磁材料
电负性
原子赝势半径
Oxide superconductor
Rare earth
Permanent magnet ma terial
Electronegativities
Atomic pseudoradii