DYNAMICS OF CU RELEASE DURING EARLY AEROBIC DEGRADATION IN AGGREGATEDSESTON FROM THE ELBE ESTUARY

Citation
M. Kerner et Cd. Geisler, DYNAMICS OF CU RELEASE DURING EARLY AEROBIC DEGRADATION IN AGGREGATEDSESTON FROM THE ELBE ESTUARY, Marine chemistry, 51(2), 1995, pp. 133-144
Citations number
58
Categorie Soggetti
Oceanografhy,Chemistry
Journal title
ISSN journal
03044203
Volume
51
Issue
2
Year of publication
1995
Pages
133 - 144
Database
ISI
SICI code
0304-4203(1995)51:2<133:DOCRDE>2.0.ZU;2-7
Abstract
Using a new laboratory device, the mobilization of Cu, Cd, and Pb was monitored continuously by analysing the water overlying and underlying a approximate to 1 mm seston layer using voltammetric methods. The mi neralization of organic matter was quantified by the heterotrophic oxy gen consumption. The CO2 formed was analysed for its C-13-content to c haracterize the organic C-pool used in degradation. Changes in the bio chemical composition of the particulate material were determined at th e beginning and end of an aerobic incubation period. Heterotrophic pro cesses were initiated about 20 h after settling of the seston. The agg regated seston became refractory for aerobic microbial degradation aft er about 120 h of aerobic incubation. At this stage nitrification agai n balanced the total oxygen consumption. The mineralization of the org anic matter was between 7.7 and 17.4% of the total and 62-75% of this consisted of dying algal biomass. A significant release of Cu from the seston layer was restricted to a period of about 40 h and was correla ted to the period when a limitation of heterotrophic processes by orga nic substrates occurred. Then, Cu concentrations increased to between 8 and 28 nM in the water overlying the layer that equalled a mobilizat ion rate of between 0.24 and 0.94 (nmol/cm(2) d). Cd and Pb did not sh ow a similar pattern and were detected at concentrations of always bel ow 2 nM. Deeper parts of the layer functioned as a sink for Cu at oxyg en concentrations of less than or equal to 25 mu M and concentrations of Cu in the water underlying the seston layer remained below 1.5 nM. During periods of short-term release Cu in solution accounted for betw een 3 and 10% of the total particulate Cu. The results suggest that a significant amount of the Cu within the seston material was retained i n the protein fraction of the algal matter and is released into the ov erlying water during its aerobic degradation.