This preprint was under review for the journal ESD but the revision was not accepted.
Radon monitoring as a possible indicator of tectonic events
V. I. Outkin1,I. A. Kozlova1,A. K. Yurkov1,P. K. Dutta2,O. P. Mishra3,4,and M. K. Naskar2V. I. Outkin et al. V. I. Outkin1,I. A. Kozlova1,A. K. Yurkov1,P. K. Dutta2,O. P. Mishra3,4,and M. K. Naskar2
1Institute of geophysics, Ekaterinburg, Amundsen Str. 100, 620016 Yekaterinburg, Russia
2Electronics and Tele-Communication Dept. Jadavpur University, 700032 Kolkata, West Bengal, India
3SAARC Disaster Management Centre (SDMC), IIPA Campus, Ring Road Delhi, 110002 Delhi, India
4Geo-seismology Division, Geological Survey of India (CHQ), Kolkata, India
1Institute of geophysics, Ekaterinburg, Amundsen Str. 100, 620016 Yekaterinburg, Russia
2Electronics and Tele-Communication Dept. Jadavpur University, 700032 Kolkata, West Bengal, India
3SAARC Disaster Management Centre (SDMC), IIPA Campus, Ring Road Delhi, 110002 Delhi, India
4Geo-seismology Division, Geological Survey of India (CHQ), Kolkata, India
Received: 06 Oct 2012 – Accepted for review: 04 Jan 2013 – Discussion started: 21 Jan 2013
Abstract. The proposed work describes research into the behavior of radon (VAR-volume activity of radon) excreted from the array. Radon migration and its selection from the array depends on the porosity, permeability and fractures in the array. A drastic change in the strength of an array and reset the elastic stresses by external forces (earthquake) occurs when certain changes in the structure of the array as the compressive and tensile strength of the array.
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