2020
DOI: 10.1016/j.atmosres.2019.104838
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Characterizing atmospheric controls on winter urban pollution in a topographic basin setting using Radon-222

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Cited by 18 publications
(9 citation statements)
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“…Radon can reach the atmosphere also from ground waters, natural gas, oceans and because of human’s activities. Due to its properties, atmospheric radon (outdoor radon), measured as radon concentration in air (Bq m −3 ), radon flux measured in radon exhaled per surface unit and per time unit (Bq m −2 s −1 ) and radon in soil gas (Bq m −3 ) are used in different scientific disciplines: (1) as a tracer gas for the estimation of greenhouse gases [ 1 , 2 , 3 , 4 , 5 , 6 ]; (2) to investigate mixing processes in the atmospheric boundary layer and the evolution of air pollution [ 7 , 8 , 9 , 10 , 11 , 12 ]; (3) as a tracer for dynamic processes such as: volcanic activity and earthquake prediction, caves air exchange, groundwater movements [ 13 , 14 , 15 , 16 , 17 , 18 , 19 , 20 , 21 ]; (4) as a tracer of Non-Aqueous Phase Liquids (NAPL) contamination [ 22 ]; (5) to estimate the health risk due to exposure to radon and its progeny [ 23 , 24 ].…”
Section: Introductionmentioning
confidence: 99%
“…Radon can reach the atmosphere also from ground waters, natural gas, oceans and because of human’s activities. Due to its properties, atmospheric radon (outdoor radon), measured as radon concentration in air (Bq m −3 ), radon flux measured in radon exhaled per surface unit and per time unit (Bq m −2 s −1 ) and radon in soil gas (Bq m −3 ) are used in different scientific disciplines: (1) as a tracer gas for the estimation of greenhouse gases [ 1 , 2 , 3 , 4 , 5 , 6 ]; (2) to investigate mixing processes in the atmospheric boundary layer and the evolution of air pollution [ 7 , 8 , 9 , 10 , 11 , 12 ]; (3) as a tracer for dynamic processes such as: volcanic activity and earthquake prediction, caves air exchange, groundwater movements [ 13 , 14 , 15 , 16 , 17 , 18 , 19 , 20 , 21 ]; (4) as a tracer of Non-Aqueous Phase Liquids (NAPL) contamination [ 22 ]; (5) to estimate the health risk due to exposure to radon and its progeny [ 23 , 24 ].…”
Section: Introductionmentioning
confidence: 99%
“…The correlation of C Rn-out with T out is weakly negative ( r = 0.34), and of C Rn-out with the pressure time gradient (∆ P /∆ t ) in the hourly scale is very weakly negative ( r = 0.09). A high correlation was not expected because outdoor 222 Rn concentration is a sum of local (exhalation from the ground) and synoptic (remote) sources [ 15 ]. The contribution of each source was not sought because, in this study, only the outdoor 222 Rn concentration during the ventilation of the apartment was needed for the simulations.…”
Section: Resultsmentioning
confidence: 99%
“…222 Rn is primarily formed by the α-transformation of radium ( 226 Ra) in the earth’s crust, from where it migrates towards the surface via diffusion and advection and exhales in the atmosphere. In general, outdoor radon concentrations are low (about 10 Bq m −3 ) [ 13 ], depending on the geological characteristics of the terrain and the atmospheric mixing state [ 14 , 15 ]. On the other hand, indoor radon concentrations are usually higher by one order of magnitude (up to several 100 Bq m −3 ) or even more (up to several 1000 Bq m −3 ).…”
Section: Introductionmentioning
confidence: 99%
“…Hourly variations of simulated and observed mixing ratios for NO x and O 3 are illustrated in Figure . Analysis of SO 2 simulation results are included in the Supporting Information (Figures S6–S8) because it was not the primary species impacting PM 2.5 concentrations in SLV during PCAPs. , There were clear day-of-week patterns of NO x concentrations in the observations, that is, high on weekdays and low on weekends. The weekly maximum NO x concentration was enhanced during PCAP events.…”
Section: Resultsmentioning
confidence: 99%