Water, Air, and Soil Pollution

, Volume 157, Issue 1, pp 107–116

Study of Aerosol Deposition at a Wind Exposed Forest Edge Using 210Pb and 137Cs Soil Inventories


    • School of PhysicsEdinburgh University
  • D. Fowler
    • Centre for Ecology and Hydrology
  • M.V. Moghaddam
    • School of PhysicsEdinburgh University

DOI: 10.1023/B:WATE.0000038879.99600.69

Cite this article as:
Branford, D., Fowler, D. & Moghaddam, M. Water, Air, & Soil Pollution (2004) 157: 107. doi:10.1023/B:WATE.0000038879.99600.69


The radionuclide 210Pb derived from gaseous 222Rn present in the atmosphere becomes attached to the same aerosols as the bulk of the main pollutants sulphur and nitrogen. When scavenged from the atmosphere by precipitation, the 210Pb is readily attached to organic matter in the surface horizons of the soil. Inventories of 210Pb in soil can thus be used to measure the spatial variations in wet (or cloud) deposition due to orography averaged over many precipitation events (half-life of 210Pb is 22.3 yr). Similar arguments apply to 137Cs inventories (half-life 30.0 yr), although more care has to be taken in interpreting the results due to possible resuspension and migration of the 137Cs. The method has been applied to quantify the long-term enhancement in aerosol and cloud water (occult) deposition as a consequence of increased aerodynamic roughness at an exposed forest canopy in the Highlands of Scotland. The specific activities of 210Pb and 137Cs in dried soil samples were determined by γ-spectrometry using HpGe detectors, one of which was fitted with a Compton suppression shield. Measurements revealed an average canopy enhancement in deposition of 36 ± 12% relative to the open heathland, in agreement with independent measurements of occult deposition at similar sites and model estimates. Deposition at the exposed edge exceeds that in the open by ≳50%, and thus provides evidence of a pronounced edge effect.

acid rainaerosol deposition137Csdry depositionoccult deposition210Pbradioactive tracerssurface roughness effects

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© Kluwer Academic Publishers 2004