HEAVY-METAL CONCENTRATIONS IN PLANTS IN RELATION TO ATMOSPHERIC HEAVY-METAL DEPOSITION

Citation
Bo. Berthelsen et al., HEAVY-METAL CONCENTRATIONS IN PLANTS IN RELATION TO ATMOSPHERIC HEAVY-METAL DEPOSITION, Journal of environmental quality, 24(5), 1995, pp. 1018-1026
Citations number
37
Categorie Soggetti
Environmental Sciences
ISSN journal
00472425
Volume
24
Issue
5
Year of publication
1995
Pages
1018 - 1026
Database
ISI
SICI code
0047-2425(1995)24:5<1018:HCIPIR>2.0.ZU;2-E
Abstract
Zinc, Cu, Ph, and Cd concentrations were examined in several plant spe cies and corresponding organic topsoil collected in forest and on ombr otrophic bogs along a temporal (1982-1992) and a spatial (Southern Nor way-Central Norway) heavy metal deposition gradient. This allowed rela tions between metal concentrations in plants, soil/peat, peat, and spa tial and temporal changes in atmospheric deposition of heavy metals to be studied. Lead concentrations in plants decreased significantly fro m 1982 to 1992 both in Southern and Central Norway, while stable level s were observed in surface soil. These observations together with a de crease in atmospheric Pb deposition rates of about 70% both in Souther n and Central Norway, suggests that direct atmospheric deposition stro ngly influenced Pb levels in vegetation. Lead concentrations in vegeta tion were significantly higher in Southern Norway than in Central Norw ay both in 1982 and 1992, evidently due to a more than 15 times higher Pb deposition in Southern Norway. Plant concentrations of Zn, Cu, and Cd were significantly higher in Southern Norway than in Central Norwa y, both in 1982 and 1992, most likely because of higher root uptake in Southern Norway due to distinctly higher surface soil levels of Zn, C u, and Cd from air pollution in this region. No distinct changes in Zn , Cu, or Cd concentrations in plants, however, where observed from 198 2 to 1992, even in Southern Norway where wet deposition of these eleme nts decreased by about 26% (Zn), 40% (Cu), and 51% (Cd) during this pe riod.