Abstract
The main aims of this study were to determine whether reservoir sediments provide good temporal records of atmospherically deposited spheroidal carbonaceous particles (SCPs), and to examine their spatial distribution within the reservoir. SCPs are produced solely by fossil-fuel burning and are good indicators of the extent of industrial pollution.
The site chosen for the study was Drasov Reservoir in the Czech Republic. Sediment cores were taken along two transects within the reservoir.
The results suggest that wind- and inlet-induced currents have an important influence on both SCP and sediment distribution in the reservoir, and that the distribution of SCPs is different to that of sediments. The SCP records were most reliable in the down-wind area of the reservoir, and although most detailed SCP record was contained in a deep-water core near the dam, records in shallower-water cores from the down-wind side of the reservoir were also good.
The correlation between SCP accumulation rates and solid emissions from local sources was very good (Spearman R=0.867, p=0.001).