Abstract
A technique for studying long-term radon anomalies is proposed. It is intended for anomalies originating from a impulse of the radon concentration generated in a center of destruction during the period of its activation. This technique has been used for quantitative interpretation of experimental data during determination of the spatiotemporal characteristics of a center of destruction and parameters of radon migration.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
