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Radon originating from meta-volcanics located at the bottom of Bossea karstic mountain aquifer is subject to transport within the cave through both advective and diffusive processes. According to the double convective cell model of circulation referable to this hypogeal atmosphere, it is possible to correlate radon fluctuations with hydrodynamics,...
Radon originating from meta-volcanics located at the bottom of Bossea karstic mountain aquifer is subject to transport within the cave through both advective and diffusive processes. According to the double convective cell model of circulation referable to this hypogean atmosphere, it is possible to correlate radon fluctuations with hydrodynamics,...