Till sidans topp

Sidansvarig: Webbredaktion
Sidan uppdaterades: 2012-09-11 15:12

Tipsa en vän
Utskriftsversion

Intercalibration of benth… - Göteborgs universitet Till startsida
Webbkarta
Till innehåll Läs mer om hur kakor används på gu.se

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

Artikel i vetenskaplig tidskrift
Författare Anders Tengberg
Per Hall
U Andersson
Bengt Lindén
O Styrenius
G Boland
F de Bovee
B. Carlsson
S Ceradini
A Devol
G. Duineveld
Jens-Uwe Friemann
R. N. Glud
A. Khripounoff
J. Leather
P. Linke
L. Lund-Hansen
G. Rowe
P. Santschi
P. de Wilde
U. Witte
Publicerad i Marine Chemistry
Volym 94
Nummer/häfte 1-4
Sidor 147-173
Publiceringsår 2005
Publicerad vid Institutionen för kemi
Sidor 147-173
Språk en
Länkar dx.doi.org/10.1016/j.marchem.2004.0...
Ämnesord 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
Ämneskategorier Kemi

Sammanfattning

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.

Sidansvarig: Webbredaktion|Sidan uppdaterades: 2012-09-11
Dela:

På Göteborgs universitet använder vi kakor (cookies) för att webbplatsen ska fungera på ett bra sätt för dig. Genom att surfa vidare godkänner du att vi använder kakor.  Vad är kakor?