Lessons Learnt from Monitoring the Etna Volcano Using an IoT Sensor Network through a Period of Intense Eruptive Activity.

This paper describes the successes and failures after 4 years of continuous operation of a network of sensors, communicating nodes, and gateways deployed on the Etna Volcano in Sicily since 2019, including a period of Etna intense volcanic activity that occurred in 2021 and resulted in over 60 paroxysms. It documents how the installation of gateways at medium altitude allowed for data collection from sensors up to the summit craters. Most of the sensors left on the volcanic edifice during winters and during this period of intense volcanic activity were destroyed, but the whole gateway infrastructure remained fully operational, allowing for a very fruitful new field campaign two years later, in August 2023. Our experience has shown that the best strategy for IoT deployment on very active and/or high-altitude volcanoes like Etna is to permanently install gateways in areas where they are protected both from meteorological and volcanic hazards, that is mainly at the foot of the volcanic edifice, and to deploy temporary sensors and communicating nodes in the more exposed areas during field trips or in the summer season.

What can gross alpha/beta activities tell about 210Po and 210Pb in the atmosphere?

210Po and 210Pb represent the most abundant part of atmospheric aerosol long-lived natural radioactivity. Moreover, 210Pb-210Po monitoring in the atmosphere can be of interest for tracking extreme natural events that can enhance the level of alpha/beta radioactivity in air. In this paper, we question the possibility to use routine gross alpha/beta measurements in order to monitor 210Po, 210Pb and 210Po/210Pb ratio in the atmosphere. Based on joint gross alpha/beta measurement and 210Pb-210Po specific determination on 16 atmosphere samples, we show that (i) gross beta activity systematically overestimates 210Pb activity due to the presence of interfering beta emitters and (ii) gross alpha activity mostly reflects 210Po activity even if an underestimation is always observed due to alpha particle attenuation in the sample. In order to determine 210Po/210Pb ratio, we discuss the advantages of using gross alpha activity time variation compared to specific 210Po measurements. Finally, the gross alpha/beta ratio appear to be a good proxy of the 210Po/210Pb ratio when large-scale variations are to be monitored. We report a first reference level for the activity level of airborne 210Po in France of 13 ± 6 µBq/m3.

From Sensor to Cloud: An IoT Network of Radon Outdoor Probes to Monitor Active Volcanoes.

While radon in soil gases has been identified for decades as a potential precursor of volcanic eruptions, there has been a recent interest for monitoring radon in air on active volcanoes. We present here the first network of outdoor air radon sensors that was installed successfully on Mt. Etna volcano, Sicily, Italy in September 2019. Small radon sensors designed for workers and home dosimetry were tropicalized in order to be operated continuously in harsh volcanic conditions with an autonomy of several months. Two stations have been installed on the south flank of the volcano at ~3000 m of elevation. A private network has been deployed in order to transfer the measurements from the stations directly to a server located in France, using a low-power wide-area transmission technology from Internet of Things (IoT) called LoRaWAN. Data finally feed a data lake, allowing flexibility in data management and sharing. A first analysis of the radon datasets confirms previous observations, while adding temporal information never accessed before. The observed performances confirm IoT solutions are very adapted to active volcano monitoring in terms of range, autonomy, and data loss.