Diel variation of arsenic,molybdenum and antimony in a stream draining natural As geochemical anomaly |
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| Institution: | 1. Department of Civil, Environmental and Architectural Engineering, University of Genoa, Genoa, Italy;2. Departmento de Ambiente e Ordenamento, University of Aveiro, 3810-193 Aveiro, Portugal;3. School of the Environment, University of Dundee, Dundee DDI 4HN, United Kingdom;4. Department of Geography, University of Hull, Hull HU6 7RX, United Kingdom;5. Department of Civil, Architectural and Environmental Engineering, University of Padua, 35131 Padua, Italy |
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| Abstract: | The Mokrsko Stream in the central Czech Republic is an oxic and slightly alkaline stream that drains a natural As geochemical anomaly. Although long-term monitoring has characterized the general seasonal trends in trace element concentrations (i.e., As, Mo, Cu, Zn) in this stream, little is known about solubility controls and sorption processes that influence diel cycles in trace element concentrations. Trace elements (including As species, Cu, Mn, Mo, Pb and Sb) and other parameters were monitored over two 24-h periods in unfiltered and filtered (0.1 μm) samples collected in August 2010 and June 2011. Copper and Pb were predominantly (>92% of the mass) associated with the particulate fraction (>0.1 μm). Arsenic, Mo and Sb were predominantly (>88% of the mass) in the “dissolved” (<0.1 μm) form. Particulate-associated elements displayed up to a factor of 13 differences between minimum and maximum concentrations, most likely due to increased streamflow related to rainfall events. Dissolved concentrations of the trace metal cations (Cu, Fe, Mn and Pb) were consistently low and displayed no diel trends. Dissolved As(V), Mo and Sb varied on a diel cycle, with increased concentrations (up to 36%) during the late afternoon and decreased concentrations during the nighttime. Diel trends in trace anionic elements are explained by temperature-dependent sorption, as the diel changes in pH during base flow were very small (0.07 std. units). Very low concentrations of As(III), which have been shown to vary in a diel cycle, were attributed to enhanced hydraulic exchange with As(III)-rich hyporheic water during rainfall events. |
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