The estimation of radon progeny in the Arctic re- gion represents a scientific challenge due to the required low limit of detection in consideration of the limited radon em- anation associated with permafrost dynamics. This prelim- inary study highlighted, for the first time above 70 o N, the possibility to monitor radon progeny in the Arctic region with a higher time resolution. The composition of the radon progeny offered the opportunity to identify air masses domi- nated by long-range transport, in presence or absence of near- constant radon progeny instead of long- and short-lived pro- genies. Furthermore, the different ratio between radon and thoron progenies evidenced the contributions of local emis- sions and atmospheric stability. Two different emanation pe- riods were defined in accordance with the permafrost dynam- ics at the ground and several accumulation windows were recognized coherently to the meteo-climatic conditions oc- curring at the study site.

High time-resolved radon progeny measurements in the Arctic region (Svalbard islands, Norway): results and potentialities

Roberto Salzano;Antonello Pasini;Antonietta Ianniello;Mauro Mazzola;
2018

Abstract

The estimation of radon progeny in the Arctic re- gion represents a scientific challenge due to the required low limit of detection in consideration of the limited radon em- anation associated with permafrost dynamics. This prelim- inary study highlighted, for the first time above 70 o N, the possibility to monitor radon progeny in the Arctic region with a higher time resolution. The composition of the radon progeny offered the opportunity to identify air masses domi- nated by long-range transport, in presence or absence of near- constant radon progeny instead of long- and short-lived pro- genies. Furthermore, the different ratio between radon and thoron progenies evidenced the contributions of local emis- sions and atmospheric stability. Two different emanation pe- riods were defined in accordance with the permafrost dynam- ics at the ground and several accumulation windows were recognized coherently to the meteo-climatic conditions oc- curring at the study site.
2018
Radon progeny
Svalbard islands
Arctic
atmospheric stability
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/371910
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