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Geochemistry of surface sediments of a coastal Lake Sarbsko (northern
Poland)
Michał Woszczyk1, Roman
Cieśliński2, Waldemar Spychalski3
1 Department of Quaternary Geology &
Palaeogeography, Adam Mickiewicz University,
Dzięgielowa 27, 61-680 Poznań, Poland,
e-mail: woszczyk@amu.edu.pl
2 Department of Hydrology, Gdańsk University, R.
Dmowskiego 16a, 80-264 Gdańsk, Poland, e-mail: georc@univ.gda.pl
3 Department of Soil Science, Poznań University
of Life Sciences, Szydłowska 50, 60-656 Poznań, Poland, e-mail: spychal@au.poznan.pl
Abstract
The main goal of the presented research was to
investigate spatial distribution of surface sediments and to recognize relationships
between chemical composition of water and sediments in a coastal Lake Sarbsko
(northern Poland).
The Lake Sarbsko is a freshwater basin. The water
column is well oxygenated and waters exhibit only minor spatial variability of
chemical composition indicating rapid and good mixing. Surface sediments of Lake Sarbsko
are strongly diversified with respect to chemical composition. The sediments of Lake Sarbsko
are characterized by elevated content of terrigenous silica indicating enhanced
input of clastic material from the watershed and/or increased dynamics of the
lake waters. Moreover, SiO2ter is strongly negatively correlated
with SiO2biog, organic matter and element contents, which argues for diluting effect
of the former towards authigenic components of sediments. Basically,
terrigenous silica (quartz) content is highest in the lake shores and declines
towards the lake center. Biogenic silica, organic matter and most of elements
display reversed tendency. CaCO3 was encountered in three
isolated areas, where it co-occurs with FeS.
It is anticipated that precipitation of calcite in Lake Sarbsko
resulted from postdepositional processes. Spatial distribution of Fe, Mn, Ca,
Mg, Na and K in Lake
Sarbsko is also governed
by their geochemical affinities to organic matter (Fe), Fe/Mn oxides (Fe, Mn),
sulphides (Fe), clay minerals (Na, K, Mg, Mn) and carbonates (Ca, Mn).
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