Characterization of precipitation-induced radon progeny deposition events using a city-scale sensor network

TL;DR

This study analyzes how precipitation affects radon progeny deposition in urban environments using a city-scale sensor network, revealing consistent relationships and categorizing precipitation events to improve radiological anomaly detection.

Contribution

It introduces a detailed characterization of rain-induced radon progeny deposition events and proposes meteorological-based background models for enhanced detection accuracy.

Findings

Power-law relationship between radon progeny proxy and NMF component peak

Identification of three distinct precipitation event categories based on radon levels

Case study linking high radon progeny levels to Wyoming uranium-rich air masses

Abstract

Networks of radiation detectors provide a platform for real-time radioactive source detection and identification in urban environments. Detection algorithms in these systems must adapt to naturally-occurring changes in background, which requires well-characterized relationships between precipitation events and their corresponding radiological signature. We present a description of rain-induced radon progeny deposition events occurring in Chicago from September 2023 through February 2024. We measure ambient gamma radiation levels, precipitation rate, temperature, pressure and relative humidity in a network of sensor nodes. For each identified precipitation period, we decompose spectra into static- and radon-associated components as defined by a non-negative matrix factorization (NMF) algorithm. We find a consistent power-law relationship between a precipitation-dependent peak of the radon progeny proxy (RPP) and the peak strength of radon-associated NMF component for most precipitation events. We conduct a case study of a rainfall period with abnormally high levels of implied radon progeny concentration and describe its temporal and spatial evolution. We hypothesize this phenomenon is due to the air mass path that intersects a uranium-rich region of Wyoming. Finally, we cluster precipitation events into three distinct categories. One category roughly corresponds to events with deep low-pressure systems and high relative radon concentration, while another is characteristic of light stratiform rain with slightly higher temperatures and intermediate relative radon concentration. The third category contains a weak-gradient or lake breeze convection showers with intermittent precipitation and low relative radon concentration. These findings suggest that radiological anomaly detection could be improved by training unique background models corresponding to each category of meteorological event.