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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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摘要

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Japan Materials Testing Reactor(JMTR)的离子束加速器和裂变反应器中,在可见光波长范围和1000至3000 nm范围内测量了稀土氧化物材料的放射发光。在氧化er中,通过质子束照射观察到在560、660和1540nm处的峰,并且通过质子束照射以及在50MW的反应堆全功率操作下观察到在1800nm和2000nm附近的复杂的发光峰。 560、660和1540 nm处的峰归因于Er〜(3+)离子能级之间的电子跃迁。 JMTR中观察到的复杂的发光随着照射时间的消逝而消失,尽管强度不受2.6 x 10〜(13)p / cm〜2s的质子束照射的影响而改变。据认为,在中子辐照下,在1800和2000 nm附近出现复杂发光峰的前体消失了。

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