Radiolead (210Pb) and stable lead in the lichen Cladonia alpestris
(1974) In Oikos 25(2). p.140-147- Abstract
Lichens of the genus Cladonia, mainly C. alpestris, collected during 1882-1972 were analyzed for stable lead and 210Pb. The specific activity of 210Pb (210Pb/Pb ratio) indicates a constant value of about 2 mCi/kg up to 1940, and then decreased to 0.6 mCi/kg during 1950-1960. As the average annual 210Pb deposition is relatively constant, the decrease in the 210Pb/Pb ratio after 1940 indicates an increased deposition of stable lead after 1940. A single exponential variation of the 210Pb/Pb ratio, in respect to latitude, was found in lichens collected in 1964. Values for 210Pb and stable lead in C. alpestris, collected in central Sweden during 1961-1972, appear to... (More)
Lichens of the genus Cladonia, mainly C. alpestris, collected during 1882-1972 were analyzed for stable lead and 210Pb. The specific activity of 210Pb (210Pb/Pb ratio) indicates a constant value of about 2 mCi/kg up to 1940, and then decreased to 0.6 mCi/kg during 1950-1960. As the average annual 210Pb deposition is relatively constant, the decrease in the 210Pb/Pb ratio after 1940 indicates an increased deposition of stable lead after 1940. A single exponential variation of the 210Pb/Pb ratio, in respect to latitude, was found in lichens collected in 1964. Values for 210Pb and stable lead in C. alpestris, collected in central Sweden during 1961-1972, appear to be relatively constant and the average area content of 210Pb and stable lead in lichen carpets was 15 ± 2 nCi/m2 and 25 ± 5 mg/m2 respectively. The pattern of vertical distribution was converted to a model for the translocation of lead in lichens, which included the diffusion principle. The diffusion coefficient for lead in the top layer of the lichen carpet was estimated to be about (0.2 ± 0.1) x 10-6 cm2 x s-1.
(Less)
- author
- Persson, B. R.R. LU ; Liden, K. and Holm, Elis LU
- organization
- publishing date
- 1974-01-01
- type
- Contribution to journal
- publication status
- published
- in
- Oikos
- volume
- 25
- issue
- 2
- pages
- 8 pages
- publisher
- Wiley-Blackwell
- external identifiers
-
- scopus:0016230595
- ISSN
- 0030-1299
- DOI
- 10.2307/3543635
- language
- English
- LU publication?
- yes
- id
- 7f21482e-e57a-4d96-8af1-e01c5420f0b8
- date added to LUP
- 2020-08-30 21:11:59
- date last changed
- 2021-01-04 11:04:27
@article{7f21482e-e57a-4d96-8af1-e01c5420f0b8, abstract = {{<p>Lichens of the genus Cladonia, mainly C. alpestris, collected during 1882-1972 were analyzed for stable lead and <sup>210</sup>Pb. The specific activity of <sup>210</sup>Pb (<sup>210</sup>Pb/Pb ratio) indicates a constant value of about 2 mCi/kg up to 1940, and then decreased to 0.6 mCi/kg during 1950-1960. As the average annual <sup>210</sup>Pb deposition is relatively constant, the decrease in the <sup>210</sup>Pb/Pb ratio after 1940 indicates an increased deposition of stable lead after 1940. A single exponential variation of the <sup>210</sup>Pb/Pb ratio, in respect to latitude, was found in lichens collected in 1964. Values for <sup>210</sup>Pb and stable lead in C. alpestris, collected in central Sweden during 1961-1972, appear to be relatively constant and the average area content of <sup>210</sup>Pb and stable lead in lichen carpets was 15 ± 2 nCi/m<sup>2</sup> and 25 ± 5 mg/m<sup>2</sup> respectively. The pattern of vertical distribution was converted to a model for the translocation of lead in lichens, which included the diffusion principle. The diffusion coefficient for lead in the top layer of the lichen carpet was estimated to be about (0.2 ± 0.1) x 10-<sup>6</sup> cm<sup>2</sup> x s-<sup>1</sup>.</p>}}, author = {{Persson, B. R.R. and Liden, K. and Holm, Elis}}, issn = {{0030-1299}}, language = {{eng}}, month = {{01}}, number = {{2}}, pages = {{140--147}}, publisher = {{Wiley-Blackwell}}, series = {{Oikos}}, title = {{Radiolead (<sup>210</sup>Pb) and stable lead in the lichen Cladonia alpestris}}, url = {{http://dx.doi.org/10.2307/3543635}}, doi = {{10.2307/3543635}}, volume = {{25}}, year = {{1974}}, }