Luminescence of non-bridging oxygen hole centers as a marker of particle irradiation of {\alpha}-quartz
Linards Skuja, Nad\`ege Ollier, Koichi Kajihara

TL;DR
This study investigates the luminescence properties of non-bridging oxygen hole centers in quartz, proposing their potential as markers for particle irradiation exposure, with specific spectral and lifetime characteristics distinguishing them from other luminescence bands.
Contribution
It demonstrates that NBOHC photoluminescence in quartz can serve as a selective marker for particle irradiation exposure, differentiating it from other luminescence signals.
Findings
NBOHC luminescence is induced by neutron and electron irradiation in quartz.
Distinct lifetime and vibrational features identify NBOHC-related luminescence.
NBOHC luminescence can be used to detect particle irradiation history in quartz.
Abstract
The origin of the "red" emission bands in the 600 nm-700 nm region, observed in quartz crystals used for luminescence dating and environmental dosimetry, is still controversial. Their reported spectral and lifetime characteristics are often similar to those of oxygen dangling bonds ("non-bridging oxygen hole centers, NBOHCs") in glassy silicon dioxide. The presence of these "surface radical type" centers in quartz crystal requires sites with highly disordered local structure forming nano-voids characteristic to the structure of glassy SiO2. Such sites are introduced in the tracks of nuclear particles ({\alpha}-irradiation, neutrons, ions). In case of electrons they are created only at large doses (>5 GGy), approaching amorphization threshold. This study reports a comparison of NBOHC photoluminescence in synthetic quartz and silica glass irradiated by neutrons or 2.5 MeV electrons, and…
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