A Whole-Basin Study of Sediment Accumulation Using Stable Lead Isotopes and Flyash Particles in an Acidified Lake, Sweden

• Published in: Limnology and oceanography Vol. 46; no. 1; pp. 178 - 188
• Main Authors: Bindler, Richard, Renberg, Ingemar, Brannvall, Maja-Lena, Emteryd, Ove, El-Daoushy, Farid
• Format: Journal Article
• Language: English
• Published: Waco, TX American Society of Limnology and Oceanography 01-01-2001
• Subjects: Atmospherics; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Freshwater; Isotope geochemistry; Isotope geochemistry. Geochronology; Isotope ratios; Isotopes; Marine and continental quaternary; Pollution, environment geology; Radioactive water pollution; Sediment contamination; Sediments; Soil pollution; Surficial geology; Sweden, Haersvatten L; Water depth; Water pollution; Watersheds; Scandinavia; Sweden; Sweden, Vaestra Goetaland, Haersvatten L; particulate matters; drill cores; lake sediments; modern; Europe; carbonaceous composition; organic materials; Pb-207/Pb-206; acidification; lakes; pollution; sedimentation rates
• ISSN: 0024-3590; 1939-5590
• DOI: 10.4319/lo.2001.46.1.0178

Using analyses of lead concentrations, lead isotopes (206Pb/207Pb), and spheroidal carbonaceous flyash particles (SCP), we studied sediment accumulation patterns in the acidified lake Harsvatten in southwest Sweden. After determining the natural background206Pb/207Pb ratio (1.5) in deeper sediments in long sediment cores from three basins in the lake, we applied an isotope mixing model to quantify pollution Pb accumulation in 46 gravity cores. The mean pollution Pb inventory in the cores was 2.6 g m-2(range, 0.3-11 g m-2). Although some variation in Pb concentrations can be explained by loss on ignition (LOI) and water depth (together, R2
adj= 0.33), there is no relationship between pollution Pb inventories and these variables. Contrary to the traditional model of sediment focusing, where higher accumulations of pollutants are expected in deeper waters, the highest inventories for pollution Pb and SCP are generally found at shallow sites ($<$4 m water depth) and not in the three deep basins of the lake (10, 12, and 24 m deep). Furthermore, the model for sediment focusing, which may be appropriate for describing the physical building of sediments in a lake basin, may be inappropriate for describing the specific processes controlling the distribution of pollutants in a lake basin of this type.