天然方钠石中的电偶极中心和色心

W.E. Van Den Brom, J. Kerssen, J. Volger
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引用次数: 8

摘要

描述了在天然矿物方钠石中表现出多重弛豫的电偶极子中心的实验。偶极中心的浓度在X射线照射下降低,而同时出现色中心和顺磁中心。热漂白可恢复原来的浓度。这些中心之间的相互关系已经确立。提出了一个模型,其中偶极中心归因于间隙单价金属离子(比如Na+离子),作为Al3+离子的电荷补偿器,取代Si4+离子。这种Al-Na络合物可能被X射线破坏,产生一个被捕获在钠离子处的电子和一个被困在与Al3+离子相邻的非桥氧离子处的空穴,X射线诱导中心的光学和顺磁性质都归因于此。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Electric dipole centres and colour centres in natural sodalite

Experiments on an electric dipole centre, exhibiting multiple relaxation, in the natural mineral sodalite, are described. The concentration of the dipole centres is reduced upon X irradiation, whereas simultaneously colour centres and paramagnetic centres arise. Thermal bleaching restores the original concentrations. The interrelationships between these centres are established.

A model is proposed in which the dipole centre is ascribed to an interstitial monovalent metal ion (say a Na+ ion) acting as a charge compensator for an Al3+ ion, substituted for a Si4+ ion. This Al-Na complex may be destroyed by X rays, yielding an electron trapped at the sodium ion and a hole trapped at a nonbridging oxygen ion, adjacent to the Al3+ ion, to which both the optical and paramagnetic properties of the X ray induced centres are attributed.

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