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WFRF:(Hulth Stefan 1965)
 

Sökning: WFRF:(Hulth Stefan 1965) > Macrofaunal reworki...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003497naa a2200517 4500
001oai:gup.ub.gu.se/56212
003SwePub
008240528s2004 | |||||||||||000 ||eng|
024a https://gup.ub.gu.se/publication/562122 URI
024a https://doi.org/10.1016/j.seares.2004.02.0022 DOI
040 a (SwePub)gu
041 a eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Caradec, S.4 aut
2451 0a Macrofaunal reworking activities and hydrocarbon redistribution in an experimental sediment system
264 1b Elsevier BV,c 2004
520 a The influence of macrofaunal reworking activities on the redistribution of particle associated hydrocarbon compounds (HC) was experimentally investigated. Two distinct hydrocarbon mixtures adsorbed on montmorillonite particles (< 4 gm diameter) were added to the surface and deeper (2.5 cm) sediment layers. For comparison, luminophores (100-160 mum diameter) were added in the two deposit layers. At the start of the experiment, four macrobenthic species (the bivalve Abra nitida, the polychaete Scalibregma inflatum, and the echmoderms Amphiura filiformis and Echinocardium cordatum) were added to the sediment surface. The macrofauna added rapidly transferred HC from the surface sediment down to similar to5 cm depth by both continuous (biodiffusion) and non-continuous (biotransport) transport. Hydrocarbon compounds initially added to the deeper sediment layer were only subject to biodiffusion-like transport. Apparent biodiffusion coefficients (Db) quantified by using a 1-D model were between 0.5 and 8.4 x 10(-3) cm(2) d(-1), and biotransport coefficients (r) ranged from 2.0 to 27.6 X 10(-3) d(-1). Thus, the four species studied did not have the same effect on particle redistribution and, consequently, on HC repartition in the sediments. E. cordatum was the most efficient reworker. The present study demonstrated the importance of particle size selectivity by benthic fauna, and verified that macrofaunal reworking activities may redeposit sediment from deeper sediment layers on the sediment surface. Both processes have obvious implications for rates and pathways during organic matter mineralisation in marine sediments. (C) 2004 Elsevier B.V. All rights reserved.
650 7a NATURVETENSKAPx Kemi0 (SwePub)1042 hsv//swe
650 7a NATURAL SCIENCESx Chemical Sciences0 (SwePub)1042 hsv//eng
653 a bioturbation
653 a hydrocarbons
653 a sediment reworking
653 a macrofauna
653 a Gullmar
653 a Fjord
653 a DEPOSIT FEEDERS
653 a MARINE SEDIMENT
653 a ORGANIC-MATTER
653 a CHLOROPHYLL-A
653 a BIOTURBATION
653 a PARTICLE
653 a FATE
653 a DEGRADATION
653 a CARBON
653 a QUANTIFICATION
700a Grossi, V.4 aut
700a Hulth, Stefan,d 1965u Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry4 aut0 (Swepub:gu)xhulst
700a Stora, G.4 aut
700a Gilbert, F.4 aut
710a Göteborgs universitetb Institutionen för kemi4 org
773t Journal of Sea Researchd : Elsevier BVg 52:3, s. 199-210q 52:3<199-210x 1385-1101
856u https://hal.archives-ouvertes.fr/hal-00757304/file/Gilbert_6099.pdf
8564 8u https://gup.ub.gu.se/publication/56212
8564 8u https://doi.org/10.1016/j.seares.2004.02.002

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Caradec, S.
Grossi, V.
Hulth, Stefan, 1 ...
Stora, G.
Gilbert, F.
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