Abstract
Soil–gas radon time series data has been generated at Dharamshala station for seismic studies in NW Himalayas, India. Compared with the influence of temperature and pressure, radon and rainfall have shown a strong correlation. Decomposition of radon time series into three component series (seasonal, trend, and residual) has been done for further recognizing the authentic anomalous values. The irregular patterns in daily and residual radon data have been associated with earthquake events and rainfall. This monitoring station found to be sensitive to the seismic events within a distance of about 70 km.
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References
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Acknowledgements
Authors thankfully acknowledge the financial support from the Himachal Pradesh Council for Science Technology and Environment (HIMCOSTE) for undertaking this joint study of HIMCOSTE and the Government Post Graduate College Dharamshala as part of the R&D program of HIMCOSTE. The India Meteorological Department (IMD), the Government of India for providing necessary meteorological and seismological data used in this study are also acknowledged.
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Dhar, S., Randhawa, S.S., Kumar, A. et al. Decomposition of continuous soil–gas radon time series data observed at Dharamshala region of NW Himalayas, India for seismic studies. J Radioanal Nucl Chem 327, 1019–1035 (2021). https://doi.org/10.1007/s10967-020-07575-x
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DOI: https://doi.org/10.1007/s10967-020-07575-x