Seasonal variations in soil radon emanation: long-term continuous monitoring in light of seismicity
Autor: | Semih Ergintav, M. Nuri Bodur, Sedat İnan, Hasan Cetin, Onur Tan, Alican Kop, Cemil Seyis, Ruhi Saatçılar, Zümer Pabuçcu, Furkan Kulak |
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Přispěvatelé: | Çukurova Üniversitesi |
Rok vydání: | 2012 |
Předmět: |
Hydrology
Atmospheric Science East Mediterranean Province Hydrogeology Soil gas Continuous monitoring Semi-annual variations chemistry.chemical_element East Anatolian Fault system Radon Baseline data Induced seismicity Earthquake precursor respiratory tract diseases Term (time) Southern Turkey chemistry Dead Sea Fault system Meteorological effects Natural hazard Earth and Planetary Sciences (miscellaneous) Soil radon Geology Water Science and Technology |
Zdroj: | Natural Hazards. 62:575-591 |
ISSN: | 1573-0840 0921-030X |
DOI: | 10.1007/s11069-012-0096-6 |
Popis: | Soil gas radon release patterns have been monitored continuously for more than 3 years in the Eastern Mediterranean Province (EMP) (Southern Turkey), alongside regional seismic events, providing a multidisciplinary approach. In the period from January 2008 to January 2011, 14 earthquakes M L ?4 occurred in the study area. By monitoring the sites for more than 3 years, the site-characteristic patterns of soil radon emanation of each site have become evident. Radon emanation data show seasonal (semi-annual) variation characteristics; high soil radon values are between May and October and low soil radon values are between November and April. With available rainfall data, the soil gas radon data can be more reliably evaluated. It is shown in this paper that if radon emanation data are available over sufficiently long periods of time and baseline data (and their seasonal variations) are known with certainty for each monitoring site, then the observation of positive anomalies might provide a correlation or connection to seismic activity. © 2012 Springer Science+Business Media B.V. TARAL, 105G019 Acknowledgments The authors acknowledge the financial support received from the TUBITAK TARAL 1007 Program for the TÜRDEP Project (Project No: 105G019). We appreciate all the technical help and support we have received from our colleagues at the TUBITAK Marmara Research Center Earth and Marine Sciences Institute. Special thanks go to Bora Erkan for the production of the figures. Finally, we thank three anonymous reviewers for their constructive reviews and suggestions that improved the manuscript. We acknowledge the promptness and the high quality of the work of the editorial office of the NHAZ. |
Databáze: | OpenAIRE |
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