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Intercalibration of benthic flux chambers II. Hydrodynamic characterization and flux comparisons of 14 different designs

Tengberg, Anders, 1962 (author)
Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry,University of Gothenburg
Hall, Per, 1954 (author)
Gothenburg University,Göteborgs universitet,Institutionen för kemi,Department of Chemistry,University of Gothenburg
Andersson, U (author)
Göteborgs universitet,University of Gothenburg
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Lindén, Bengt, 1956 (author)
Göteborgs universitet,University of Gothenburg
Styrenius, O (author)
Göteborgs universitet,University of Gothenburg
Boland, G (author)
de Bovee, F (author)
Centre national de la recherche scientifique (CNRS)
Carlsson, B. (author)
Chalmers tekniska högskola,Chalmers University of Technology
Ceradini, S (author)
Devol, A (author)
University of Washington
Duineveld, G. (author)
Royal Netherlands Institute for Sea Research - NIOZ
Friemann, Jens-Uwe, 1956 (author)
Chalmers tekniska högskola,Chalmers University of Technology
Glud, R. N. (author)
Köpenhamns universitet,University of Copenhagen,Texas A and M University
Khripounoff, A. (author)
IFREMER Centre de Brest
Leather, J. (author)
Linke, P. (author)
Helmholtz Zentrum,Helmholtz Center
Lund-Hansen, L. (author)
Århus Universitet,Aarhus University
Rowe, G. (author)
Santschi, P. (author)
Texas A and M University
de Wilde, P. (author)
Royal Netherlands Institute for Sea Research - NIOZ
Witte, U. (author)
Max Planck Gesellschaft zur Förderung der Wissenschaften e.V. (MPG),Max Planck Society for the Advancement of Science (MPG)
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 (creator_code:org_t)
Elsevier BV, 2005
2005
English.
In: Marine Chemistry. - : Elsevier BV. - 0304-4203. ; 94:1-4, s. 147-173
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • We have compared 14 different sediment incubation chambers, most of them were used on bottom landers. Measurements of mixing time, pressure gradients at the bottom and Diffusive Boundary Layer thickness (DBL) were used to describe the hydrodynamic properties of the chambers and sediment-water solute fluxes of silicate (34 replicates) and oxygen (23 replicates) during three subsequently repeated incubation experiments on a homogenized, macrofauna-free sediment. The silicate fluxes ranged from 0.24 to 1.01 mmol m(-2) day(-1) and the oxygen fluxes from 9.3 to 22.6 mmol m(-2) day(-1). There was no statistically significant correlation between measured fluxes and the chamber design or between measured fluxes and hydrodynamic settings suggesting that type of chamber was not important in these flux measurements. For verification of sediment homogeneity, 61 samples of meiofauna were taken and identified to major taxa. In addition. 13 sediment cores were collected. sectioned into 5-10-mm slices and separated into pore water and solid phase. The pore water profiles of disolved silicale were used to calculate diffusive fluxes of silicate. These fluxes ranged from 0.63 to 0.87 mmol m(-2) day(-1). All of the collected sediment parameters indicated that the sediment homogenization process had been satisfactorily accomplished, hydrodynamic variations inside and between chambers are a reflection of the chamber design and the stirring device, In general. pump stirrers with diffusers give a more even distribution of bottom currents and DBL thicknesses than paddle wheel-type stirrers, Most chambers display no or low static differential pressures when the water is mixed at rates of normal Use, Consequently. there is a low risk of creating stirrer induced pressure effects on the measured fluxes. Centrally placed stirrers are preferable to off-center placed stirrers which are more difficult to map and do not seem to give any hydrodynamic advantages, A vertically rotating stirrer gives about five times lower static differential pressures at the same stirring, speed as the same stirrer mounted horizontally If the aim is to simulate or mimic resuspension at high flow velocities, it cannot be satisfactorily done in a chamber using it horizontal (standing) rotating impeller (as is the case for most chambers in use) due to the creation of unnatural conditions. i,e. large static differential pressures and pre-mature resuspension at certain locations in the chamber. (c) 2004 Elsevier B.V. All rights reserved.

Subject headings

NATURVETENSKAP  -- Kemi (hsv//swe)
NATURAL SCIENCES  -- Chemical Sciences (hsv//eng)

Keyword

benthic chambers
calibration
hydrodynamic properties
comparative
flux incubations
SEDIMENT-WATER INTERFACE
DIFFUSIVE BOUNDARY-LAYERS
OXYGEN-UPTAKE
DEEP-SEA
SOLUTE TRANSPORT
PORE-WATER
IN-SITU
EXCHANGE
FLOOR
INSITU
OXYGEN-UPTAKE

Publication and Content Type

ref (subject category)
art (subject category)

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