Abstract
AbstractMercury accumulation in lake sediments is a widespread environmental problem due to the biomagnification of Hg in the aquatic food chain. Soil Hg concentrations, catchment vegetation, erosion, and lake productivity are major factors controlling the accumulation of Hg in lakes. However, their influence on the Hg mass balance in lakes with different catchment characteristics and trophic state is poorly understood. In this multilake study, we decipher the effects of catchment vegetation (coniferous vs. deciduous forest), soil Hg content, and trophic state on Hg sedimentation at six lakes in Germany. We investigated Hg concentrations in leaves, soils, and the lake's water phase. Soils under coniferous stands show slightly higher Hg concentrations than under deciduous forest. Hg concentrations in the water phase were higher in the oligotrophic brown water lakes (8.1 ± 5.6 ng L−1 vs. 3.0 ± 1.9 ng L−1). Lower Hg concentrations in sediment trap material indicate dilution by algae organic matter in the mesotrophic lakes (0.12–0.17 μg g−1 vs. 0.57–0.89 μg g−1). However, Hg accumulation rates in sediment traps were up to 14‐fold higher in the mesotrophic lakes (113–443 μg m−2 yr−1) than in the brown water lakes (32–144 μg m−2 yr−1), which could not be explained by higher Hg fluxes to the productive lakes. Hg mass balance calculation reveals that water phase Hg scavenging by algae is the major reason for the intense Hg export to the sediments of productive lakes which makes them significantly larger sedimentary sinks than oligotrophic brown water lakes.
Highlights
We investigated six lakes in two mountain areas in Germany, which differ in catchment vegetation and in-lake primary productivity
The lakes are predominantly used for flood control and local recreation, as these waterbodies are located near the provincial town of Ballenstedt (Fig. 1B) where settlements are partly downstream of the lake outflows
We compared Hg accumulation in oligotrophic brown water lakes and mesotrophic to eutrophic lakes and catchment soils at two forested areas in Germany which differ in catchment vegetation and weather conditions
Summary
Needles of evergreen coniferous trees provide a larger surface area for Hg uptake when regarding the leaf/needle surface area on an annual basis (i.e., no leaf surface area in deciduous forests in winter) (Obrist et al 2012; Navrátil et al 2014). MeHg is known to be formed in forest soils and is transported to lakes by POM and DOM (Tsz-Ki Tsui et al 2019), the role of different forest vegetation in lake catchments on water phase Hg concentrations and Hg accumulation in lake sediments is poorly understood
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