Wet Deposition of Radon-222 Progeny in Northern Finland Measured with an Automatic Precipitation Gamma Analyser

An automatic wet deposition gamma analyser has been constructed. Precipitation is collected with a 1 m2 funnel and its 214Pb and 214Bi contents measured in a Marinelli beaker with an NaI(Tl) detector and a multichannel analyser. The amount of water in the beaker is measured with an ultrasonic sensor...

Full description

Bibliographic Details
Main Author: Paatero, J.
Format: Text
Language:English
Published: Oxford University Press 2000
Subjects:
Online Access:http://rpd.oxfordjournals.org/cgi/content/short/87/4/273
id fthighwire:oai:open-archive.highwire.org:rpd:87/4/273
record_format openpolar
spelling fthighwire:oai:open-archive.highwire.org:rpd:87/4/273 2023-05-15T15:09:25+02:00 Wet Deposition of Radon-222 Progeny in Northern Finland Measured with an Automatic Precipitation Gamma Analyser Paatero, J. 2000-02-02 00:00:00.0 text/html http://rpd.oxfordjournals.org/cgi/content/short/87/4/273 en eng Oxford University Press http://rpd.oxfordjournals.org/cgi/content/short/87/4/273 Copyright (C) 2000, Nuclear Technology Publishing Article TEXT 2000 fthighwire 2007-06-24T09:54:02Z An automatic wet deposition gamma analyser has been constructed. Precipitation is collected with a 1 m2 funnel and its 214Pb and 214Bi contents measured in a Marinelli beaker with an NaI(Tl) detector and a multichannel analyser. The amount of water in the beaker is measured with an ultrasonic sensor. All the sensor and spectrum data are gathered, and the magnetic valves controlled, with a data logger and a microcomputer. The instrument was tested during a five-month field measurement campaign in northern Finland. A value of 750 Bq.1-1 for the geometric mean 222Rn progeny concentration in precipitation, and a geometric mean washout ratio of 9.1 x 105 was obtained in this study. Their variations, however, were large: four orders of magnitude. The Rn progeny concentrations and washout ratios are inversely correlated with low precipitation intensities. With higher precipitation intensities this behaviour levels out. Higher washout ratios were observed during rainfall compared to snowfall. Low Rn progeny concentrations in precipitation are usually connected with cold or occluded fronts and surges of arctic air masses. On the other hand, high Rn progeny concentrations are usually related to warm fronts or sectors. They are also observed between two successive cyclones, when continental air masses from southern Russia move northwest. The results obtained could also be applied to wet-depositing chemical substances like heavy metals, which can be difficult to measure using on-line methods. Text Arctic Northern Finland HighWire Press (Stanford University) Arctic Marinelli ENVELOPE(-62.900,-62.900,-64.267,-64.267)
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Article
spellingShingle Article
Paatero, J.
Wet Deposition of Radon-222 Progeny in Northern Finland Measured with an Automatic Precipitation Gamma Analyser
topic_facet Article
description An automatic wet deposition gamma analyser has been constructed. Precipitation is collected with a 1 m2 funnel and its 214Pb and 214Bi contents measured in a Marinelli beaker with an NaI(Tl) detector and a multichannel analyser. The amount of water in the beaker is measured with an ultrasonic sensor. All the sensor and spectrum data are gathered, and the magnetic valves controlled, with a data logger and a microcomputer. The instrument was tested during a five-month field measurement campaign in northern Finland. A value of 750 Bq.1-1 for the geometric mean 222Rn progeny concentration in precipitation, and a geometric mean washout ratio of 9.1 x 105 was obtained in this study. Their variations, however, were large: four orders of magnitude. The Rn progeny concentrations and washout ratios are inversely correlated with low precipitation intensities. With higher precipitation intensities this behaviour levels out. Higher washout ratios were observed during rainfall compared to snowfall. Low Rn progeny concentrations in precipitation are usually connected with cold or occluded fronts and surges of arctic air masses. On the other hand, high Rn progeny concentrations are usually related to warm fronts or sectors. They are also observed between two successive cyclones, when continental air masses from southern Russia move northwest. The results obtained could also be applied to wet-depositing chemical substances like heavy metals, which can be difficult to measure using on-line methods.
format Text
author Paatero, J.
author_facet Paatero, J.
author_sort Paatero, J.
title Wet Deposition of Radon-222 Progeny in Northern Finland Measured with an Automatic Precipitation Gamma Analyser
title_short Wet Deposition of Radon-222 Progeny in Northern Finland Measured with an Automatic Precipitation Gamma Analyser
title_full Wet Deposition of Radon-222 Progeny in Northern Finland Measured with an Automatic Precipitation Gamma Analyser
title_fullStr Wet Deposition of Radon-222 Progeny in Northern Finland Measured with an Automatic Precipitation Gamma Analyser
title_full_unstemmed Wet Deposition of Radon-222 Progeny in Northern Finland Measured with an Automatic Precipitation Gamma Analyser
title_sort wet deposition of radon-222 progeny in northern finland measured with an automatic precipitation gamma analyser
publisher Oxford University Press
publishDate 2000
url http://rpd.oxfordjournals.org/cgi/content/short/87/4/273
long_lat ENVELOPE(-62.900,-62.900,-64.267,-64.267)
geographic Arctic
Marinelli
geographic_facet Arctic
Marinelli
genre Arctic
Northern Finland
genre_facet Arctic
Northern Finland
op_relation http://rpd.oxfordjournals.org/cgi/content/short/87/4/273
op_rights Copyright (C) 2000, Nuclear Technology Publishing
_version_ 1766340619752439808