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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003999naa a2200505 4500
001oai:DiVA.org:su-148955
003SwePub
008171114s2017 | |||||||||||000 ||eng|
024a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1489552 URI
024a https://doi.org/10.1016/j.envpol.2017.08.0862 DOI
040 a (SwePub)su
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Mustajärvi, Lukasu Stockholms universitet,Institutionen för miljövetenskap och analytisk kemi4 aut0 (Swepub:su)lumu0844
2451 0a In situ benthic flow-through chambers to determine sediment-to-water fluxes of legacy hydrophobic organic contaminants
264 1b Elsevier BV,c 2017
338 a electronic2 rdacarrier
520 a Contaminated sediment can release hydrophobic organic contaminants (HOCs) and thereby act as a secondary source of primarily legacy hazardous substances to the water column. There is therefore a need for assessments of the release of HOCs from contaminated sediment for prioritization of management actions. In situ assessment of HOC sediment-to-water flux is currently done with (closed) benthic flux chambers, which have a sampling time exceeding one month. During this time, the water inside the chamber is depleted of oxygen and the effect of bioturbation on the sediment-to-water release of HOCs is largely ignored. Here we present a novel benthic flux chamber, which measures sediment-to-water flux of legacy HOCs within days, and includes the effect of bioturbation since ambient oxygen levels inside the chamber are maintained by continuous pumping of water through the chamber. This chamber design allows for sediment-to-water flux measurements under more natural conditions. The chamber design was tested in a contaminated Baltic Sea bay. Measured fluxes were 62–2300 ng m−2 d−1 for individual polycyclic aromatic hydrocarbons (PAHs), and 5.5–150 ng m−2 d−1 for polychlorinated biphenyls (PCBs). These fluxes were 3–23 times (PAHs) and 12–74 times (PCBs) higher than fluxes measured with closed benthic chambers deployed in parallel at the same location. We hypothesize that the observed difference in HOC flux between the two chamber designs are partly an effect of bioturbation. This hypothesized effect of bioturbation was in accordance with literature data from experimental studies.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653 a Flux
653 a Sediment
653 a Benthic chamber
653 a Bioturbation
653 a Bioirrigation
653 a Flöden
653 a sediment
653 a bottenkammare
653 a bioturbation
653 a Applied Environmental Science
653 a tillämpad miljövetenskap
700a Eek, Espen4 aut
700a Cornelissen, Gerard4 aut
700a Eriksson-Wiklund, Ann-Kristinu Stockholms universitet,Institutionen för miljövetenskap och analytisk kemi4 aut0 (Swepub:su)aerik
700a Undeman, Emmau Stockholms universitet,Stockholms universitets Östersjöcentrum4 aut0 (Swepub:su)emun5928
700a Sobek, Annau Stockholms universitet,Institutionen för miljövetenskap och analytisk kemi4 aut0 (Swepub:su)subek
710a Stockholms universitetb Institutionen för miljövetenskap och analytisk kemi4 org
773t Environmental Pollutiond : Elsevier BVg 231, s. 854-862q 231<854-862x 0269-7491x 1873-6424
856u https://doi.org/10.1016/j.envpol.2017.08.086y Fulltext
856u https://su.diva-portal.org/smash/get/diva2:1156700/FULLTEXT01.pdfx primaryx Raw objecty fulltext:print
856u https://doi.org/10.1016/j.envpol.2017.08.086
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-148955
8564 8u https://doi.org/10.1016/j.envpol.2017.08.086

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