Heavy metals in soils and plants of the don river estuary and the Taganrog Bay coast
- Autores: Minkina T.M.1, Fedorov Y.A.1, Nevidomskaya D.G.1, Pol’shina T.N.2, Mandzhieva S.S.1, Chaplygin V.A.1
-
Afiliações:
- Southern Federal University
- Institute of Arid Zones, Southern Scientific Center
- Edição: Volume 50, Nº 9 (2017)
- Páginas: 1033-1047
- Seção: Soil Chemistry
- URL: https://journals.rcsi.science/1064-2293/article/view/224148
- DOI: https://doi.org/10.1134/S1064229317070067
- ID: 224148
Citar
Resumo
Natural and anthropogenic factors determining the distribution and accumulation features of Pb, Cu, Zn, Cr, Ni, Cd, Mn, and As in the soil–plant system of the Don River estuary and the northern and southern Russian coasts of Taganrog Bay estuary have been studied. High mobility of Cu, Zn, Pb, and Cd has been revealed in alluvial soils. This is confirmed by the significant bioavailability of Cu, Zn, and, to a lesser degree, Cd and the technophily of Pb, which are accumulated in tissues of macrophytic plants. Statistically significant positive correlations have been found between the mobile forms of Cu, Zn, Cd, and Mn in the soil and the accumulation of metals in plants. Impact zones with increased metal contents in aquatic ecosystems can be revealed by bioindication from the morphofunctional parameters of macrophytic plants (with Typha L. as an example).
Palavras-chave
Sobre autores
T. Minkina
Southern Federal University
Autor responsável pela correspondência
Email: tminkina@mail.ru
Rússia, Rostov-on-Don, 344006
Yu. Fedorov
Southern Federal University
Email: tminkina@mail.ru
Rússia, Rostov-on-Don, 344006
D. Nevidomskaya
Southern Federal University
Email: tminkina@mail.ru
Rússia, Rostov-on-Don, 344006
T. Pol’shina
Institute of Arid Zones, Southern Scientific Center
Email: tminkina@mail.ru
Rússia, Rostov-on-Don, 344006
S. Mandzhieva
Southern Federal University
Email: tminkina@mail.ru
Rússia, Rostov-on-Don, 344006
V. Chaplygin
Southern Federal University
Email: tminkina@mail.ru
Rússia, Rostov-on-Don, 344006
Arquivos suplementares
