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- W2023984785 abstract "To examine the effects of atmospheric pressure fluctuations on radon entry into houses, we report measurements of soil-gas and advective radon entry made using an experimental basement. Based on these measurements, we quantify the contribution of atmospheric pressure fluctuations, steady indoor−outdoor pressure differences, and molecular dif fusion to the long-term radon entry rate into the experimental basement. In the absence of a steady indoor−outdoor pressure difference, atmospheric pressure fluctuations at the study site induce a radon entry rate 1.5 times greater than that due to molecular diffusion. A steady indoor−outdoor pressure difference reduces the contribution of atmospheric pressure fluctuations to the long-term radon entry rate. For sustained indoor−outdoor pressure differences with a magnitude greater than 1.5 Pa, atmospheric pressure fluctuations have essentially no effect on the time-averaged radon entry rate into the experimental structure. The results of this study demonstrate that under certain conditions, such as periods during which indoor−outdoor pressure differences are small, atmospheric pressure fluctuations will contribute measurably to the total radon entry rate into a building, potentially doubling indoor concentrations. However, in absolute terms, atmospheric pressure fluctuations drive approximately the same amount of entry as molecular diffusion and, therefore, will probably not cause houses to have long-term, elevated indoor radon concentrations." @default.
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- W2023984785 date "1997-05-29" @default.
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- W2023984785 title "Radon Entry into Buildings Driven by Atmospheric Pressure Fluctuations" @default.
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- W2023984785 doi "https://doi.org/10.1021/es960715v" @default.
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