Evidence map›Paper›PMID 39943572›Full record

ArticleSensors (Basel, Switzerland)2025

Spatio-Temporal Correlation Between Radon Emissions and Seismic Activity: An Example Based on the Vrancea Region (Romania).

David Montiel-López, Sergio Molina, Juan José Galiana-Merino, Igor Gómez, Alireza Kharazian, Juan Luís Soler-Llorens, José Antonio Huesca-Tortosa, Arianna Guardiola-Villora, Gonzalo Ortuño-Sáez

Abstract read
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Article in Sensors (Basel, Switzerland), 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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1 · What the graph read from it

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4 · The record

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5 · Who and what money

Authors and funding

9 authors.

David Montiel-LópezMultidisciplinary Institute for Environmental Studies, University of Alicante, Ctra. San Vicente del Raspeig, s/n, 03080 Alicante, Spain.ORCID 0000-0001-5673-4546
Sergio MolinaMultidisciplinary Institute for Environmental Studies, University of Alicante, Ctra. San Vicente del Raspeig, s/n, 03080 Alicante, Spain.ORCID 0000-0002-8909-6285
Juan José Galiana-MerinoDepartment of Physics, Systems Engineering and Signal Theory, University of Alicante, Ctra. San Vicente del Raspeig, s/n, 03080 Alicante, Spain.ORCID 0000-0002-0818-2836
Igor GómezMultidisciplinary Institute for Environmental Studies, University of Alicante, Ctra. San Vicente del Raspeig, s/n, 03080 Alicante, Spain.ORCID 0000-0002-2176-5630
Alireza KharazianMultidisciplinary Institute for Environmental Studies, University of Alicante, Ctra. San Vicente del Raspeig, s/n, 03080 Alicante, Spain.ORCID 0000-0003-2691-8875
Juan Luís Soler-LlorensDepartment of Earth and Environmental Sciences, University of Alicante, Ctra. San Vicente del Raspeig, s/n, 03080 Alicante, Spain.ORCID 0000-0003-4540-8790
José Antonio Huesca-TortosaDepartment of Architectural Constructions, University of Alicante, Ctra. San Vicente del Raspeig, s/n, 03080 Alicante, Spain.ORCID 0000-0002-0649-6575
Arianna Guardiola-VilloraDepartment of Continuum Mechanics and Theory of Structures, Universitat Politècnica de València, Camino de Vera, s/n, 46022 Valencia, Spain.ORCID 0000-0003-3234-0547
Gonzalo Ortuño-SáezIndependent Researcher, 03300 Orihuela, Spain.

Funding

Conselleria de Educación, Cultura, Universidades y Empleo de la Generalitat Valenciana CIAICO/2022/038Government of Spain (Ministry of Science, Innovation and Universities) PID2021-123135OB-C21
6 · The paper itself

Abstract

Radon gas anomalies have been investigated as potential earthquake precursors for many years. In this work, we have studied the possible correlations between radon emissions and the seismic activity rate for a given region to test if the existing correlation may be later used to forecast the occurrence of earthquakes larger than a given magnitude. The Vrancea region (Romania) was chosen as a study area since it is being surveilled by a multidisciplinary real-time monitoring network, and at least seven earthquakes with magnitudes greater than 4.5 Mw have occurred in this area in the period from 2016 to 2020. Our research followed several steps: First, the recorded radon signals were preprocessed (detrended, deseasoned and smoothed). Then, the station's signals were correlated in order to check which stations are recording radon anomalies due to the same regional tectonic process. On the other hand, the seismic activity rate was computed using the earthquakes in the main catalogue of the region that are able to generate radon emissions and can be registered at several stations. The obtained results indicate a significant correlation between the seismic activity rate and the temporal series of radon anomalies. A temporal lag between the seismic activity rate and the radon anomalies was found, which can be related to the proximity to the epicentre of the main earthquake in each of the studied subperiods. Changes in the regional tectonic stress field could explain why the seismic activity rate and radon anomalies are correlated over time. Further research could focus on obtaining a function to forecast the seismic activity rate using the following as dependent variables: the radon anomalies recorded at several stations, the distance from the stations, and tectonic factors such as the fault system, azimuth, type of soil, etc.

Indexed as

correlationearthquakelagradonRomaniaseismicitysignalVrancea

Identifiers

PMID39943572
PMCPMC11819798

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.