Abstract. Radon (222Rn) gas is the largest source of public exposure to naturally
occurring radioactivity and the identification of radon priority areas is
required by the Council Directive 2013/59/Euratom. Radon is also used as a
tracer to improve atmospheric transport models and to indirectly estimate
greenhouse gas (GHG) fluxes using the Radon Tracer Method (RTM). This method
is based on the correlation between atmospheric concentrations of radon and
GHG, together with information on the radon flux data. For radiological
data, all European countries have installed networks of automatic gamma dose
rate monitoring stations and report the real-time information gathered to
the European Radiological Data Exchange Platform (EURDEP). So far,
atmospheric radon activity concentrations and radon fluxes are not yet
reported in EURDEP, nor routinely measured within the European radiological
networks although these observations could help to avoid false positives
results. Due to above applications, there is a need of building a metrological chain
to ensure high quality radon activity concentrations and radon flux
measurements. Both climate and radiation protection research communities
underline the need for improved traceability in low-level atmospheric radon
measurements (Khanbabaee et al., 2021). The EMPIR project 19ENV01
traceRadon1 is aimed towards
providing the necessary measurement infrastructure and transfer standards to
fulfil this need. Results of this project are particularly important for improving independent
GHG emission estimates that support national reporting under the Paris
Agreement on climate change and for the Council Directive 2013/59/Euratom,
thus benefitting two large scientific communities. In this paper, early
results, such as new activity standard developments and an overview of
commercial and research radon monitors are presented and discussed. These
results will feed into the traceRadon project with respect to radionuclide
metrology in air and its potential for the improvement of the RTM.