eCite Digital Repository
The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes
Citation
Gallagher, JB, The Influence of Iron and Manganese on Nutrient Cycling in Shallow Freshwater Antarctic Lakes, Antarctic Nutrient Cycles and Food Webs, Springer-Verlag Berlin Heidelberg, WR Siegfried, PR Condy and RM Laws (ed), Germany, pp. 234-237. ISBN 9783642822773 (1985) [Research Book Chapter]
Copyright Statement
Copyright 1985 Springer-Verlag Berlin Heidelberg
Official URL: https://www.springer.com/gp/book/9783642822773
DOI: doi:10.1007/9783642822759
Abstract
Two lakes, mesotrophic Heywood Lake and oligotrophic
Sombre Lake, at Signy Island, have been studied over 1 full yr
(1980-1981). The development of deep water anoxia in Sombre
Lake is accompanied by release, from the sediments, of nitrogen,
silicon, phosphorus, iron, and manganese. Iron is released from
anoxic sediments in massive amounts, but is quickly returned
through oxidation to iron oxides, near the anoxic-<>xic boundary
and through possible ferrous carbonate precipitation, within the
anoxic region. Phosphorus is also quickly returned to sediments, at
the oxic-anoxic boundary, which suggests efficient co-precipitation-sorption
by the recently oxidized ferrous. Phosphorus is therefore
unable to enter the main waterbody. Melt water inflows are the
source of P supply to the surface waters. Nitrogen and Si appear to
have little association with axides and, therefore, freely pass into the
oxic main water-body of the oligotrophic system. There are strong
seasonal correlations between the vertical profiles of Fe and P,
under the ice cover in Heywood Lake. Nitrogen profiles appear
independent of the other determinants, Si, P, Fe, and Mn. Towards
the end of the period of bottom-water anoxia, during the spring
melt, high concentrations of ferrous, released from the anoxic
sediments, have been detected in oxygenated waters. This apparent
stability, in the presence of oxygen, may be attributable to a combination
of low pH and the possible influence of high concentrations
of humic acids from the melt inflows. Sulphide concentrations may
become sufficiently high to influence Fe transport significantly,
probably through ferrous sulphide precipitation, within the anoxic
region.
Item Details
Item Type: | Research Book Chapter |
---|---|
Keywords: | humic acid, ferric oxide, anoxic sediment, Antarctic lake, ferrous carbonate |
Research Division: | Earth Sciences |
Research Group: | Oceanography |
Research Field: | Chemical oceanography |
Objective Division: | Environmental Management |
Objective Group: | Coastal and estuarine systems and management |
Objective Field: | Assessment and management of coastal and estuarine ecosystems |
UTAS Author: | Gallagher, JB (Dr John Barry Gallagher) |
ID Code: | 136970 |
Year Published: | 1985 |
Deposited By: | Oceans and Cryosphere |
Deposited On: | 2020-01-23 |
Last Modified: | 2020-03-03 |
Downloads: | 0 |
Repository Staff Only: item control page