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The radionuclides 210 Po and 210 Pb widely present in the terrestrial environment are the final long-lived radionuclides in the decay of 238 U in the earth’s crust. Their presence in the atmosphere is due to the decay of 222 Rn diffusing from the ground. The range of activity concentrations in ground level air for 210 Po is 0.03–0.3 Bq m −3 and for ...
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