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Obtaining isochrones from pollution signals in a fluvial sediment record: A case study in a uranium-polluted floodplain of the Ploucnice River, Czech Republic

Publication at Faculty of Science |
2014

Abstract

Uranium mining and processing in the watershed of the Ploucnice River in the Czech Republic during a well-defined time interval (1969-1989) allowed for a study of pollutant fates in sediments of a meandering river that is otherwise in a nearly natural state. A considerable part of the primary pollution is present in hotspots in the floodplain 10-15 km downstream from the mining district.

One of the hotspots was characterised using geoinformatic, geophysical and geochemical means. The floodplain geomorphology and architecture and river channel dynamics were studied to develop an understanding of the formation of the hotspot and evaluate further movement of pollutants in the river system.

Local background functions (with Rb or Ti as a predictor) and local enrichment factors (LEFs) were obtained for Ba, Ni, Pb, U and Zn concentrations in unpolluted sediments from the deeper strata of the active floodplain, an abandoned floodplain and an ancient terrace. The most recent (2013) overbank fines in the study area are still considerably enriched in Ni, U and Zn (LEF 3, 6 and 8, respectively), and thus pollution by heavy metals several km downstream of the hotspots continuously increases even though the primary source of pollution was terminated more than 20 years ago.

The onset of the primary pollution is hence clearly identified in the distal floodplain sediments as persistent and a potentially isochronous pollution signal in the fluvial record, whereas a secondary pollution signal overwrites the expected "primary pollution climax'' and "pollution improvement'' signals. That inertia of the fluvial system can also be expected in other river systems with both laterally and vertically deposited sediments.

The Ploucnice case study allowed for further elaboration of the concept of local enrichment factors in pollution assessment of fluvial sediments, which efficiently reduces the grain-size effects and hence allows for reconstruction of the pollution history.