Thoron Component Of Atmospheric Radon
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Air was sampled by the use of suction pump through a glass filter (> 90% filtrationrnefficiency) and aerosols were deposited on the glass-fiber filter. The aerosol depositedrnon the filter paper was placed below a GM tube (with GM nuclear counter) within arntime interval of less than one minute after the end of sampling. The gross ¯ countsrnwere registered in successive time intervals for more than six to ten hours (i.e. inrnintervals of 1 min for the first one hour; 2 min for the second hour; 4 min for thernthird hour etc. )rnThe activity concentration of progenies of 222Rn and EEC (equilibrium equivalentrnconcentration) of 222Rn was done by fitting the observed gross ¯ count to a mathematicalrnmodel derived.rnThe indoor and outdoor variation of 222Rn was observed inside and outsidernof the nuclear physics laboratory (around four meters above the ground).rnThe average EEC of 222Rn was found to be 23.9 Bq=m3 and 3.4 Bq=m3 for indoorrnand outdoor respectively.rnIndoor radon concentration is 4 to 6 times higher than the outdoor concentration.rnOur result agrees with the results available in other studies
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Modern Geology projects now focus on Machine Learning in Mineral Targeting, Carbon Capture & Storage (CCS) Geologic Modeling, and Critical Mineral Systems (Lithium, REEs). If your research involves Hydrogeological Connectivity, Seismic Inversion, or Geotechnical Site Characterization, ensure your analysis follows the JORC or NI 43-101 reporting standards and utilizes robust 3D Subsurface Visualization and Geochemical Fingerprinting frameworks.
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