2013
Trends and evolution of contamination in a well-dated water reservoir sedimentary archive: the Brno Dam, Moravia, Czech Republic
SEDLÁČEK, Jan, Ondřej BÁBEK a Tomas Matys GRYGARZákladní údaje
Originální název
Trends and evolution of contamination in a well-dated water reservoir sedimentary archive: the Brno Dam, Moravia, Czech Republic
Autoři
SEDLÁČEK, Jan (203 Česká republika, garant, domácí), Ondřej BÁBEK (203 Česká republika, domácí) a Tomas Matys GRYGAR
Vydání
Environmental Earth Sciences, New York, Springer, 2013, 1866-6280
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10511 Environmental sciences
Stát vydavatele
Spojené státy
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 1.572
Kód RIV
RIV/00216224:14310/13:00107090
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000322390300010
Klíčová slova anglicky
Brno Dam; Dam sediments; Cs-137 dating; Heavy metals; Eutrophication
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 30. 4. 2020 13:04, Mgr. Michal Petr
Anotace
V originále
The sedimentary record from dams can provide important information about stratigraphy and pollution history of densely populated river basins. The Brno Dam is a small reservoir within the Morava River catchment (Czech Republic) accumulating lacustrine sediments since 1940 (dam filling). The stratigraphy of the dam sediments was studied using multiproxy stratigraphic analysis (X-ray densitometry, bulk magnetic susceptibility, diffuse spectral reflectance and cation-exchange capacity) of five sediment cores supported by ground-penetration radar sections. Concentrations of heavy metals were studied by X-ray fluorescence analysis. The thickness of the dam sediments decreases from 220 cm in the proximal part, near the feeder, to only 10 cm in the distal part, near the dyke. Sediments consist predominantly of finely-laminated silty sands, silts and clays. The sedimentation rate for the last similar to 22 years, inferred from Cs-137 dating, decreases from 4.2 cm per year in the proximal part of the dam to 0.29 cm per year in its distal part. Distinct long-term trends were found in the depth profiles of heavy metal concentrations. The heavy metal contents increase significantly after 1940 in all cores, with peak concentrations confined to layers deposited in the 1960s and 1980s. A decreasing trend occurred after 1989 (the decline in Czech heavy industry). The results also show that heavy metal contamination is dependent on lithology (hyperpycnal flow layers related to floods). Increased concentrations of phosphorus in the sediments indicate long-term eutrophication of the dam. Despite the recent decreasing trends in heavy metal concentrations the phosphorus contents remain high in recent years and have caused persisting problems with algal growth in the dam mentioned by previous authors.