Physical background of the development of oxygen depletion in ice-covered lakes.

Abstract:

:The effect of the heat interaction between a water column and sediments on the formation, development, and duration of existence of anaerobic zones in ice-covered lakes is estimated based on observational data from five frozen lakes located in northwestern Russia and North America. A simple one-dimensional model that describes the formation and development of the dissolved oxygen deficit in shallow ice-covered lakes is suggested. The model reproduces the main features of dissolved oxygen dynamics during the ice-covered period; that is, the vertical structure, the thickness, and the rate of increase of the anaerobic zone in bottom layers. The model was verified against observational data. The results from the verification show that the model adequately describes the dissolved oxygen dynamics in winter. The consumption rates of DO by bacterial plankton and by bottom sediments, which depend on the heat transfer through the water-sediment interface, are calculated. The results obtained allow the appearance of potentially dangerous anaerobic zones in shallow lakes and in separate lake areas, which result from thermal regime changes, to be predicted.

journal_name

Oecologia

journal_title

Oecologia

authors

Golosov S,Maher OA,Schipunova E,Terzhevik A,Zdorovennova G,Kirillin G

doi

10.1007/s00442-006-0543-8

subject

Has Abstract

pub_date

2007-03-01 00:00:00

pages

331-40

issue

2

eissn

0029-8549

issn

1432-1939

journal_volume

151

pub_type

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