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Phthalates and Nonylphenols in Roskilde Fjord

Phthalates and Nonylphenols in Roskilde Fjord

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3.3 Samples of fjord sedimentF<strong>in</strong>ally, sediment samples <strong>in</strong> the fjord was taken dur<strong>in</strong>g 1996, most ofthem <strong>in</strong> <strong>Roskilde</strong> Vig <strong>in</strong> a fan-shaped geometry near the outlet from <strong>Roskilde</strong>WWTP (map Figure 2).NSludgeamendedfieldStation 2<strong>Roskilde</strong> Vig⊗∆WWTP outletFigure 21 km<strong>Roskilde</strong>harbourLocal map of <strong>Roskilde</strong> Vig, 1:25000, show<strong>in</strong>g locations of sedimentsampl<strong>in</strong>g sites <strong>and</strong> sources.x Sampl<strong>in</strong>g sites ⊗ Sediment core∆ WWTP outlet ∇ Sludge dump<strong>in</strong>g site∇<strong>Roskilde</strong> CityThe sampl<strong>in</strong>g design is based on <strong>in</strong>vestigations carried out 1994-95 for<strong>Roskilde</strong> County Authority <strong>and</strong> <strong>Roskilde</strong> Municipality by Danish HydraulicInstitute <strong>and</strong> Water Consult. Accord<strong>in</strong>g to these reports the currentis circulat<strong>in</strong>g <strong>in</strong> the Vig ma<strong>in</strong>ly driven by the w<strong>in</strong>d, the tide play<strong>in</strong>g am<strong>in</strong>or role. The w<strong>in</strong>d is predom<strong>in</strong>antly <strong>in</strong> the West direction, lead<strong>in</strong>g toan South-East water current <strong>in</strong> the area hav<strong>in</strong>g a velocity of 2-6 cm/sec.The WWTP average outlet of waste water is 19000 m 3 /day.Some samples were taken further North <strong>in</strong> <strong>Roskilde</strong> Vig <strong>and</strong> <strong>in</strong> <strong>Roskilde</strong>Bredn<strong>in</strong>g, on the same locations as the monthly water samples. Thesediment also <strong>in</strong>cluded samples from the neighbour<strong>in</strong>g fjord Isefjord, believedto be lesser polluted, for comparison. These fjord sediment sampleswere taken by a diver. All sediment samples were taken <strong>in</strong> the upper2-5 cm of the sediment, with the exception of the core, which reached adepth of about 22 cm <strong>in</strong>to the sediment. An overview of these samples isshown <strong>in</strong> Table 4.16The sampl<strong>in</strong>g methods are described more detailed <strong>in</strong> the AnalyticalChapter.

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