Abstract
Quenching experiments are performed with pure impure crystals of Cu2O, the latter of which contained small quantities of Zn, Ni and Ag. As regards the impure crystal quenched from 950°C to room temperature, all absorption lines appearing in the yellow and the green region of its spectrum taken at 77°K shift to red. The Ag-mingled crystal shows that it is much larger in line-shift than the others, whereas it reveals very small line-shifts when slowly cooled within the above limits of temperature. The large shift is inferred to be due to numerous “complexes” which consist of Ag+-ions and Cu+-ion vacancies. As to the pure crystal rapidly cooled, its absorption spectra display slight line-shifts, sharp lines about the yellow region when observed at 4.2°K and disturbed lines of absorption in the green series, while normal lines in the yellow, their interpretations being examined.