Abstract

“Glow-in-the-dark” materials are known to practically everyone who has ever traveled by airplane or cruise ship, since they are commonly used for self-lit emergency exit signs. The green afterglow, persistent luminescence (PeL), is obtained from divalent europium doped to a synthetic strontium aluminate, but there are also some natural minerals capable of afterglow. One such mineral is hackmanite, the afterglow of which has never been thoroughly investigated, even if its synthetic versions can compete with some of the best commercially available synthetic PeL materials. Here we combine experimental and computational data to show that the white PeL of natural hackmanite is generated and controlled by a very delicate interplay between the natural impurities present. The results obtained shed light on the PeL phenomenon itself thus giving insight into improving the performance of synthetic materials.

Highlights

  • Hackmanite is a mineral with the general composition Na8Al6Si6O24(Cl,S)[2]

  • Since hackmanites are defined as being photochromic sodalites and since the photochromism is due to the disulfide group which shows orange photoluminescence, we chose such parts of the samples that showed the disulfide emission for further characterization

  • The present work marks a new advancement in the understanding of the photonic behavior of the versatile hackmanite materials as well as the persistent luminescence phenomenon in general

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Summary

Introduction

Hackmanite is a mineral with the general composition Na8Al6Si6O24(Cl,S)[2]. For consistency with previous publications, we will keep using the name hackmanite in this work. The mechanism of tenebrescence in hackmanites is established to be due to a UV stimulated electron transfer from S22− ions to chloride vacancies creating color centers that absorb in the visible range.[7] The electrons can transfer back to the disulfide if enough thermal or optical energy is given.[5,8,9]

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