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Updated: May 5, 2026

Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films
Published on: November 9, 2015
7Be, 210Pb and 137Cs concentrations in cloud water.
L Bourcier1, O Masson2, P Laj1
1Laboratoire de Météorologie Physique, Observatoire de Physique du Globe de Clermont-Ferrand, Université Blaise Pascal - CNRS, 24 avenue des Landais, 63 177 Aubière Cedex, France.
This study measured natural radionuclides (beryllium-7 and lead-210) and cesium-137 in cloud water. Findings provide crucial data for assessing radionuclide wet deposition, especially after nuclear events.
Area of Science:
- Environmental Science
- Atmospheric Chemistry
- Radiochemistry
Background:
- Cloud water composition is vital for understanding atmospheric deposition.
- Radionuclide monitoring is essential for assessing environmental contamination, particularly post-nuclear events.
Purpose of the Study:
- To determine the concentrations of beryllium-7 (7Be), lead-210 (210Pb), and cesium-137 (137Cs) in cloud water.
- To establish a reference level for 137Cs in cloud water, representing long-term post-accidental background.
- To compare radionuclide deposition in cloud water versus rainwater and assess aerosol scavenging efficiencies.
Main Methods:
- Cloud water sampling over 8 months (2008-2009) at a high-altitude atmospheric research station.
- Measurement of activity concentrations for 7Be, 210Pb, and 137Cs using established radiometric techniques.
- Calculation of cloud-to-rain concentration ratios and aerosol scavenging efficiencies.
Main Results:
- Average activity concentrations: 7Be (1.9±0.11 mBq m⁻³ air), 210Pb (140±10 μBq m⁻³ air), and 137Cs (0.14±0.02 μBq m⁻³ air).
- The measured 137Cs level indicates a long-term post-Chernobyl accident background.
- Cloud-to-rain concentration ratios ranged from 3.4 to 8.1, while aerosol scavenging efficiencies were low (0.13-0.40).
Conclusions:
- This study provides the first reference data for 137Cs in cloud water.
- Cloud water radionuclide concentrations are significant for assessing wet deposition, especially in high-altitude regions and during fog events.
- Lower scavenging efficiencies for aerosols by cloud droplets were observed compared to soluble inorganic ions.
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