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Airborne radionuclides in mosses collected at different latitudes
M Krmar1, K Wattanavatee, D Radnović
1University Novi Sad, Trg Dositeja Obradovica, Novi Sad, Serbia. krmar@df.uns.ac.rs
Journal of Environmental Radioactivity
|September 2, 2011
Summary
Terrestrial mosses effectively monitor airborne radionuclides. Moss samples from Thailand and Serbia showed significant differences in beryllium-7 (7Be) and lead-210 (210Pb) concentrations, indicating regional deposition variations.
Area of Science:
- Environmental Science
- Radiochemistry
- Atmospheric Science
Background:
- Terrestrial mosses are ideal bioindicators for airborne radionuclide deposition.
- Their widespread distribution and ease of sampling facilitate environmental monitoring.
- High-resolution gamma spectrometry can be performed without extensive sample preparation.
Purpose of the Study:
- To compare activity concentrations of beryllium-7 (7Be), lead-210 (210Pb), and cesium-137 (137Cs) in moss samples.
- To investigate airborne radionuclide deposition in two distinct climate zones: southern Thailand (7°N) and Serbia (~45°N).
Main Methods:
- Collection of terrestrial moss samples from Thailand and Serbia.
- Analysis of radionuclide activity concentrations (Bq/kg) using high-resolution gamma spectrometry.
- Statistical comparison of (7)Be, (210)Pb, and (137)Cs levels between the two locations.
Main Results:
- A significant difference in (210)Pb content was observed, with concentrations nearly double between the two sites.
- Mean (7)Be activity in Serbian moss samples was approximately 40% higher than in Thai samples.
- (137)Cs levels in Thailand mosses were below the detection limit.
Conclusions:
- Mosses effectively reflect regional differences in airborne radionuclide deposition.
- Atmospheric transport, particularly in areas with water droplets and turbulence, can influence the deposition of uranium (U) and thorium (Th) daughter nuclei.
- The study highlights the utility of mosses for comparative environmental monitoring across diverse geographical regions.
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