VLIZ
VLAAMS INSTITUUT VOOR DE ZEE
MARIEN EN KUSTGEBONDEN ONDERZOEK & BELEID IN VLAANDEREN
   
© VLIZ © VLIZ © VLIZ © VLIZ © VLIZ
 
 
  English  Sitemap  Print
U bent hier: VLIZ > datacentrum
menu1 Over het VLIZ menu2 Infoloket menu3 Zeebibliotheek menu4 Cijfers&Beleid menu5 Faciliteiten menu6 Datacentrum
   
Datacentrum
  - IMIS: Integrated Marine Information System -
log in

Personen | Instituten | Publicaties | Projecten | Datasets | Kaarten
meld een fout in dit recordmandje (0): toevoegen | tonen Print-vriendelijke versie

Effect of oxygen on the degradability of organic matter in subtidal and intertidal sediments of the North Sea area
Dauwe, B.; Middelburg, J.J.; Herman, P.M.J. (2001). Effect of oxygen on the degradability of organic matter in subtidal and intertidal sediments of the North Sea area, in: (2001). VLIZ Coll. Rep. 31(2001). VLIZ Collected Reprints: Marine and Coastal Research in Flanders, 31: pp. chapter 18 [Subsequent publication]
In: (2001). VLIZ Coll. Rep. 31(2001). VLIZ Collected Reprints: Marine and Coastal Research in Flanders, 31. Flanders Marine Institute (VLIZ): Oostende, meer
In: VLIZ Collected Reprints: Marine and Coastal Research in Flanders. Vlaams Instituut voor de Zee: Oostende. ISSN 1376-3822, meer

Ook gepubliceerd als
  • Dauwe, B.; Middelburg, J.J.; Herman, P.M.J. (2001). Effect of oxygen on the degradability of organic matter in subtidal and intertidal sediments of the North Sea area Mar. Ecol. Prog. Ser. 215: 13-22, meer

Beschikbaar in Auteurs | Dataset 
    VLIZ: Open Repository 98987 [ OMA ]

Trefwoorden
    Degradatie; Getijsedimentatie; Organisch materiaal; ANE, Noordzee [gazetteer]; Marien

Auteurs  Top | Dataset 

Abstract
    The effect of oxygen on the degradation of sedimentary organic matter has been determined for 6 subtidal stations and 3 intertidal stations in the North Sea area. The stations were selected to cover a range of organic matter lability and sediment texture (and hence concentrations of organic matter). Slurry incubations revealed that at low mineralisation rates, aerobic mineralisation is significantly faster than anaerobic mineralisation, irrespective of the degree of lability of organic matter. A complementary incubation experiment with sediment rich in organic carbon mixed with varying proportions of organically poor sediments confirmed the enhanced aerobic mineralisation at low mineralisation levels. It is proposed that oxygen-enhanced degradation occurs at low mineralisation levels at which bacterial biomass production becomes limiting.

Dataset:
  • Effect of oxygen on the degradability of organic matter in subtidal and intertidal sediments of the North Sea area, meer

 Top | Auteurs | Dataset 
 

 

Vlaams Instituut voor de Zee
InnovOcean site
Wandelaarkaai 7
B-8400 OOSTENDE, België
Tel: +32 [0]59/34 21 30
Fax: +32 [0]59/34 21 31
Email: info@vliz.be
   

 

Vlaamse Gemeenschap Provincie West-Vlaanderen