Site-selective mapping of metastable states using electron-beam induced luminescence microscopy

TL;DR

This study employs high-resolution cathodoluminescence microscopy to map and analyze metastable electron-trapping states in feldspar, revealing spatial variability and geochemical influences on NIR emissions, advancing understanding of defect states in minerals.

Contribution

It introduces a novel spectrally-resolved cathodoluminescence microscopy method for site-specific mapping of metastable states in feldspar, challenging existing models of emission origins.

Findings

NIR emissions vary spatially and originate from different sites.

NIR emission peaks are linked to geochemical variations.

Fe4+ ions quench the NIR emission.

Abstract

Metastable states created by electron or hole capture in crystal defects are widely used in dosimetry and photonic applications. Feldspar, the most abundant mineral in the Earth crust (>50%), generates metastable states with lifetimes of millions of years upon exposure to ionizing radiation. Although feldspar is widely used in dosimetry and geochronometry, the creation of metastable states and charge transfer across them is poorly understood. Understanding such phenomena requires next-generation methods based on high-resolution, site-selective probing of the metastable states. Recent studies using site-selective techniques such as photoluminescence (PL), and radioluminescence (RL) at 7 K have revealed that feldspar exhibits two near-infrared (NIR) emission bands peaking at 880 nm and 955 nm, which are believed to arise from the principal electron-trapping states. Here, we map for the first time the electron-trapping states in potassium-rich feldspar using spectrally-resolved cathodoluminescence microscopy at a spatial resolution of around 6 to 22 micrometer. Each pixel probed by a scanning electron microscope provides us a cathodoluminescence spectrum (SEM-CL) in the range 600-1000 nm, and elemental data from energy-dispersive x-ray (EDX) spectroscopy. We conclude that the two NIR emissions are spatially variable and, therefore, originate from different sites. This conclusion contradicts the existing model that the two emissions arise from two different excited states of a principal trap. Moreover, we are able to link the individual NIR emission peaks with the geochemical variations (K, Na and Fe concentration), and propose a cluster model that explains the quenching of the NIR emission by Fe4+.