Published 2004
| Version v1
Journal article
Indoor gamma radiation and radon concentrations in a Norwegian carbonatite area
Creators
Description
Results of indoor gamma radiation and radon measurements in 95 wooden dwellings located in a Norwegian thorium-rich carbonatite area using thermoluminescent dosemeters and CR-39 alpha track detectors, respectively, are reported together with a thorough analysis of the indoor data with regard to geological factors. Slightly enhanced radium levels and thorium concentrations of several thousands Bq kg-1 in the carbonatites were found to cause elevated indoor radon-222 levels and the highest indoor gamma dose rates ever reported from wooden houses in Norway. An arithmetic mean indoor gamma dose rate of 200 nGy h-1 and a maximum of 620 nGy h-1 were obtained for the group of dwellings located directly on the most thorium-rich bedrock
Additional details
Identifiers
- DOI
- 10.1016/j.jenvrad.2004.03.007;
- PII
- S0265931X04001043;
Publishing Information
- Journal Title
- Journal of Environmental Radioactivity
- Journal Volume
- 77
- Journal Issue
- 2
- Journal Page Range
- p. 175-189
- ISSN
- 0265-931X
- CODEN
- JERAEE
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 36022015
- Subject category
- S61: RADIATION PROTECTION AND DOSIMETRY; S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- DOSE RATES; HOUSES; INDOOR AIR CONTAMINATION; NORWAY; PARTICLE TRACKS; RADIOECOLOGICAL CONCENTRATION; RADIUM; RADON; RADON 222; THERMOLUMINESCENT DOSEMETERS; THORIUM
- Descriptors DEC
- ACTINIDES; ALKALINE EARTH METALS; ALPHA DECAY RADIOISOTOPES; BUILDINGS; CONTAMINATION; DAYS LIVING RADIOISOTOPES; DEVELOPED COUNTRIES; DOSEMETERS; ECOLOGICAL CONCENTRATION; ELEMENTS; EUROPE; EVEN-EVEN NUCLEI; FLUIDS; GASES; HEAVY NUCLEI; ISOTOPES; LUMINESCENT DOSEMETERS; MEASURING INSTRUMENTS; METALS; NONMETALS; NUCLEI; RADIOISOTOPES; RADON ISOTOPES; RARE GASES; RESIDENTIAL BUILDINGS; SCANDINAVIA; WESTERN EUROPE
Optional Information
- Copyright
- Copyright (c) 2004 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.