Variability of present and past PAH concentrations in sediments of the SW Barents Sea
Permanent lenke
https://hdl.handle.net/10037/8837Dato
2015-10-09Type
Journal articleTidsskriftartikkel
Peer reviewed
Sammendrag
The concentration and distribution of polyaromatic hydrocarbons (PAHs) in surface and subsurface sediment samples from Tromsøflaket and
Ingøydjupet, southwestern Barents Sea, were investigated in order to provide insight into the levels and origins of PAHs in a region with petroleum
activities. PAH profiles in sediments were evaluated in context with sediment grain size and total organic carbon in order to assess the influence of
ocean currents on the transportation and deposition of PAHs. The PAH concentrations are of background (Level I) to good level (Level II) based on
the Water Framework Directive classification system. SUM PAH (SUM of 26 PAH compounds) ranged from 39 to 2197 µg/kg (average 225 µg/kg), and
NPD (naphthalene, phenanthrene and dibenzothiophene, including their C1–C3 alkyl homologues) in surface samples ranged from 14 to 2045 µg/kg
(average 157 µg/kg). However, the average values presented here are higher than have been reported in previous studies. The observed changes in PAH
contents in surface and subsurface sediments vary in accordance with changes in grain size (clay and silt 17–99%) and total organic carbon content
(0.37–0.98%). In turn, these sedimentary parameters are controlled by the inflow of Atlantic Water and the strength of the two predominating current
systems in this region: the North Atlantic Current and Norwegian Coastal Current. Source-allocation modeling suggests that PAHs in surface samples
are mainly of pyrogenic or mixed pyrogenic and petrogenic origin. Taken together, these patterns of PAH levels and sources reflect natural variability,
indicating that the derived dataset establishes a pre-impacted baseline of the present state of the seafloor.
Beskrivelse
Published version. Source at http://www.geologi.no/index.php/norwegian-journal-of-geology-91/details/1/538-538.