Mercury Distribution in the Deûle River (Northern France) Measured by the Diffusive Gradients in Thin Films Technique and Conventional Methods

The distribution of mercury in surface water and in sediment from Deûle River in Northern France was studied by application of conventional sampling methods and by diffusive gradients in thin films technique (DGT). Concentration of total dissolved mercury in surface water was 20.8 ± 0.8 ng l⁻¹. The...

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Veröffentlicht in:Archives of environmental contamination and toxicology 2016-05, Vol.70 (4), p.700-709
Hauptverfasser: Diviš, Pavel, Kadlecová, Milada, Ouddane, Baghdad
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Ouddane, Baghdad
description The distribution of mercury in surface water and in sediment from Deûle River in Northern France was studied by application of conventional sampling methods and by diffusive gradients in thin films technique (DGT). Concentration of total dissolved mercury in surface water was 20.8 ± 0.8 ng l⁻¹. The particulate mercury concentration was 6.2 ± 0.6 µg g⁻¹. The particulate mercury was accumulated in sediment (9.9 ± 2.3 mg kg⁻¹), and it was transformed by methylating bacteria to methylmercury, mainly in the first 2-cm layer of the sediment. Total dissolved concentration of mercury in sediment pore water obtained by application of centrifugation extraction was 17.6 ± 4.1 ng l⁻¹, and it was comparable with total dissolved pore water mercury concentration measured by DGT probe containing Duolite GT-73 resin gel (18.2 ± 4.3 ng l⁻¹), taking the sediment heterogeneity and different principles of the applied methods into account. By application of two DGT probes with different resin gels specific for mercury, it was found that approximately 30 % of total dissolved mercury in sediment pore water was present in labile forms easy available for biota. The resolution of mercury DGT depth profiles was 0.5 cm, which allows, unlike conventional techniques, to study the connection of the geochemical cycle of mercury with geochemical cycles of iron and manganese.
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Concentration of total dissolved mercury in surface water was 20.8 ± 0.8 ng l⁻¹. The particulate mercury concentration was 6.2 ± 0.6 µg g⁻¹. The particulate mercury was accumulated in sediment (9.9 ± 2.3 mg kg⁻¹), and it was transformed by methylating bacteria to methylmercury, mainly in the first 2-cm layer of the sediment. Total dissolved concentration of mercury in sediment pore water obtained by application of centrifugation extraction was 17.6 ± 4.1 ng l⁻¹, and it was comparable with total dissolved pore water mercury concentration measured by DGT probe containing Duolite GT-73 resin gel (18.2 ± 4.3 ng l⁻¹), taking the sediment heterogeneity and different principles of the applied methods into account. By application of two DGT probes with different resin gels specific for mercury, it was found that approximately 30 % of total dissolved mercury in sediment pore water was present in labile forms easy available for biota. 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Concentration of total dissolved mercury in surface water was 20.8 ± 0.8 ng l⁻¹. The particulate mercury concentration was 6.2 ± 0.6 µg g⁻¹. The particulate mercury was accumulated in sediment (9.9 ± 2.3 mg kg⁻¹), and it was transformed by methylating bacteria to methylmercury, mainly in the first 2-cm layer of the sediment. Total dissolved concentration of mercury in sediment pore water obtained by application of centrifugation extraction was 17.6 ± 4.1 ng l⁻¹, and it was comparable with total dissolved pore water mercury concentration measured by DGT probe containing Duolite GT-73 resin gel (18.2 ± 4.3 ng l⁻¹), taking the sediment heterogeneity and different principles of the applied methods into account. By application of two DGT probes with different resin gels specific for mercury, it was found that approximately 30 % of total dissolved mercury in sediment pore water was present in labile forms easy available for biota. The resolution of mercury DGT depth profiles was 0.5 cm, which allows, unlike conventional techniques, to study the connection of the geochemical cycle of mercury with geochemical cycles of iron and manganese.</abstract><cop>New York</cop><pub>Springer US</pub><pmid>26428003</pmid><doi>10.1007/s00244-015-0231-y</doi><tpages>10</tpages></addata></record>
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subjects Analysis
Analytical chemistry
Bacteria
Biota
Brackish
Centrifugation
Chemical Sciences
Concentration (composition)
Contaminated sediments
Continental interfaces, environment
Dissolution
Earth and Environmental Science
Earth Sciences
Ecotoxicology
Environment
Environmental Chemistry
Environmental Health
Environmental Monitoring - methods
Food chains
France
gels
Geochemical cycles
Geochemistry
Heterogeneity
iron
Laboratories
Lead
Manganese
Mercury
Mercury (metal)
Mercury - analysis
Metals
Methylmercury
methylmercury compounds
Monitoring/Environmental Analysis
Planetary probes
Pollution
Pore water
Porosity
Production capacity
Rivers
Sampling methods
Sciences of the Universe
Sediments
Soil Science & Conservation
Studies
Surface water
Thin films
Water Pollutants, Chemical - analysis
Water pollution
title Mercury Distribution in the Deûle River (Northern France) Measured by the Diffusive Gradients in Thin Films Technique and Conventional Methods
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