Exploring atmospheric radon with airborne gamma-ray spectroscopy
Marica Baldoncini, Matteo Alb\'eri, Carlo Bottardi, Brian Minty,, Kassandra G.C. Raptis, Virginia Strati, Fabio Mantovani

TL;DR
This study demonstrates the first use of airborne gamma-ray spectroscopy to quantify atmospheric radon, revealing its vertical distribution and concentration, which has implications for environmental health and climate research.
Contribution
It introduces a novel application of AGRS for measuring atmospheric radon levels and profiles, expanding its use beyond background radiation estimation.
Findings
Detected atmospheric radon with AGRS for the first time.
Measured radon concentration as 0.96 ± 0.07 Bq/m³.
Estimated atmospheric layer depth as 1318 ± 22 m.
Abstract
Rn is a noble radioactive gas produced along the U decay chain, which is present in the majority of soils and rocks. As Rn is the most relevant source of natural background radiation, understanding its distribution in the environment is of great concern for investigating the health impacts of low-level radioactivity and for supporting regulation of human exposure to ionizing radiation in modern society. At the same time, Rn is a widespread atmospheric tracer whose spatial distribution is generally used as a proxy for climate and pollution studies. Airborne gamma-ray spectroscopy (AGRS) always treated Rn as a source of background since it affects the indirect estimate of equivalent U concentration. In this work the AGRS method is used for the first time for quantifying the presence of Rn in the atmosphere and assessing its vertical…
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