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

IoT LoRaWAN data lake radon sensors volcano monitoring wireless sensor networks

Journal

Sensors (Basel, Switzerland)
ISSN: 1424-8220
Titre abrégé: Sensors (Basel)
Pays: Switzerland
ID NLM: 101204366

Informations de publication

Date de publication:
12 May 2020
Historique:
received: 31 03 2020
revised: 28 04 2020
accepted: 08 05 2020
entrez: 16 5 2020
pubmed: 16 5 2020
medline: 16 5 2020
Statut: epublish

Résumé

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.

Identifiants

pubmed: 32408560
pii: s20102755
doi: 10.3390/s20102755
pmc: PMC7294423
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Subventions

Organisme : CAP 20-25
ID : unknown
Organisme : ClerVolc
ID : unknown

Références

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Auteurs

Luca Terray (L)

Laboratoire de Physique de Clermont, Université Clermont Auvergne, CNRS/IN2P3, 63000 Clermont-Ferrand, France.
Laboratoire Magmas et Volcans, Université Clermont Auvergne, CNRS/INSU, 63000 Clermont-Ferrand, France.

Laurent Royer (L)

Laboratoire de Physique de Clermont, Université Clermont Auvergne, CNRS/IN2P3, 63000 Clermont-Ferrand, France.

David Sarramia (D)

Laboratoire de Physique de Clermont, Université Clermont Auvergne, CNRS/IN2P3, 63000 Clermont-Ferrand, France.

Cyrille Achard (C)

Laboratoire de Physique de Clermont, Université Clermont Auvergne, CNRS/IN2P3, 63000 Clermont-Ferrand, France.

Etienne Bourdeau (E)

Université Clermont Auvergne, Mésocentre, DSI, 63000 Clermont-Ferrand, France.

Patrick Chardon (P)

Laboratoire de Physique de Clermont, Université Clermont Auvergne, CNRS/IN2P3, 63000 Clermont-Ferrand, France.

Alexandre Claude (A)

Laboratoire de Physique de Clermont, Université Clermont Auvergne, CNRS/IN2P3, 63000 Clermont-Ferrand, France.

Jérôme Fuchet (J)

Université Clermont Auvergne, Mésocentre, DSI, 63000 Clermont-Ferrand, France.

Pierre-Jean Gauthier (PJ)

Laboratoire Magmas et Volcans, Université Clermont Auvergne, CNRS/INSU, 63000 Clermont-Ferrand, France.

David Grimbichler (D)

Université Clermont Auvergne, Mésocentre, DSI, 63000 Clermont-Ferrand, France.

Jérémy Mezhoud (J)

Université Clermont Auvergne, Mésocentre, DSI, 63000 Clermont-Ferrand, France.

Francis Ogereau (F)

Université Clermont Auvergne, Mésocentre, DSI, 63000 Clermont-Ferrand, France.

Richard Vandaële (R)

Laboratoire de Physique de Clermont, Université Clermont Auvergne, CNRS/IN2P3, 63000 Clermont-Ferrand, France.

Vincent Breton (V)

Laboratoire de Physique de Clermont, Université Clermont Auvergne, CNRS/IN2P3, 63000 Clermont-Ferrand, France.

Classifications MeSH