Distinct defect centers at oxygen positions in albite
Distinct defect centers at oxygen positions in albite
复制标题
钠长石中氧位置的明显缺陷中心
作者:
I. Petrov;A. Agel;S. Hafner
Metastable electron-hole centers in single crystals of Amelia albite were studied using electron paramagnetic resonance at 9.2 GHz between 5 and 260 K. Six distinct O' centers were identified as four Ot-/227A|centers, one O1-/27A1 x 223Na center, and one O1-/[Si,M2*] center. Values of their g and A tensors and limits of thermal stabilities were determined. The four Ot-/227 Alcenters could be assigned to Alt,,o,4.,o,-Altr(-), Alrr(o)-OD(o)-Alr2(-), Alr2(o)-Oc(-)-Alr,,-,, and Alrzlo;-Oo1-y-Alt,1-1 bridges (violations of the rule of Loewenstein) and are designated as co, do, c, and d, respectively. Their total concentration was estimated to be 2 x l0-4 to 3 x l0-4 per formula unit NaAlSi3Or. Their spectra could be observed between 5 and 220 K, the maximum intensities being near T^: 60 K. They were destroyed after heating at 523 K for 3 h. The calculated density of the O'- (2p) unpaired electron at the tetrahedral Al position is about 0.006 e. The Or-/'ziAl x 223Na center could be assigned to a Sitr,o,-Oo,-Alt,r-r bridge and is designated as ai. Its estimated concentration is at least I x lO-a per formula unit. The spectrum could be observed between 20 and 120 K, T^ - ll0 K. It was destroyed after heating at 493 K for 3 h. The O' (2ps) unpaired electron