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Infrared luminescence of rare earth oxide materials

机译:稀土氧化物材料的红外发光

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Radioluminescence from rare earth oxide materials was measured in the visible wavelength range and the range from 1000 to 3000 nm in an ion beam accelerator and a fission reactor of Japan Materials Testing Reactor (JMTR). In erbium oxide, peaks at 560, 660, and 1540 nm were observed by the proton beam irradiation, and the complicated luminescence peaks around 1800 and 2000 nm were observed by the proton beam irradiation and at the reactor full power operation of 50 MW. The peaks at 560, 660, and 1540 nm are attributed to the electron transition between the energy levels of Er~(3+) ions. The complicated luminescences observed in JMTR were quenched with the irradiation time elapsed, though the intensity was not changed by the irradiation of the proton beam of 2.6 x 10~(13) p/cm~2s. It was considered that the precursors for the complicated luminescent peaks around 1800 and 2000 nm disappeared under the neutrons irradiation.
机译:在可见波长范围内测量来自稀土氧化物材料的辐射发光,在离子束加速器和日本材料检测反应器(JMTR)的裂变反应器中的1000至3000nm的范围内测量。在氧化铒中,通过质子束照射观察560,660和1540nm的峰,通过质子束照射观察到约1800和2000nm的复杂发光峰值,并在50mW的反应器全功率操作中观察到约1800和2000nm。 560,660和1540nm处的峰值归因于ER〜(3+)离子的能量水平之间的电子转变。在JMTR中观察到的复杂发光,通过经过的照射时间淬灭,尽管强度不会通过2.6×10〜(13)p / cm〜2s的质子束的照射而改变。被认为是复杂发光峰的前体约为1800和2000nm的中子照射在中子辐照下消失。

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