Quantified Hypoxia and Anoxia in Lakes and Reservoirs

Hypoxia and anoxia occur frequently in freshwater systems and have biological and chemical implications. Anoxia can be expressed and quantified as the anoxic factor; hypoxia, for a specific level of oxygen depletion, can be expressed as the hypoxic factor in lakes, reservoirs, and river sections. Th...

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Main Author: Gertrud K. Nürnberg
Format: Article
Language:English
Published: Hindawi Limited 2004-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1100/tsw.2004.5
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spelling doaj-968ef13692804bd4b80c7c3f9ddada282020-11-25T02:19:12ZengHindawi LimitedThe Scientific World Journal1537-744X2004-01-014425410.1100/tsw.2004.5Quantified Hypoxia and Anoxia in Lakes and ReservoirsGertrud K. Nürnberg0Freshwater Research, Baysville, Ontario, CanadaHypoxia and anoxia occur frequently in freshwater systems and have biological and chemical implications. Anoxia can be expressed and quantified as the anoxic factor; hypoxia, for a specific level of oxygen depletion, can be expressed as the hypoxic factor in lakes, reservoirs, and river sections. These methods summarize information of individual dissolved oxygen profiles as annual values or factors that facilitate comparison between and within lakes. Therefore, these factors are useful in the formulation and testing of hypotheses related to the dissolved oxygen status in water bodies. Methods of calculating different factors for different oxygen levels and water layers, including those applying separately to the epilimnion and hypolimnion, are presented in detail. Proven and potential applicability include: (1) the quantification of relationships with lake water quality variables and lake classification (trophic state), (2) the evaluation of restoration techniques with respect to their effects on hypolimnetic oxygen depletion, (3) the determination of internal phosphorus loading in stratified and polymictic lakes, (4) the exploration of habitat constraints due to hypoxia (e.g., fish species richness and winterkill), (5) forecasting potential effects of climatic change on oxygen content and internal phosphorus loading, and (6) the establishment and examination of criteria and guidelines with respect to hypoxia by custom-made definitions.http://dx.doi.org/10.1100/tsw.2004.5
collection DOAJ
language English
format Article
sources DOAJ
author Gertrud K. Nürnberg
spellingShingle Gertrud K. Nürnberg
Quantified Hypoxia and Anoxia in Lakes and Reservoirs
The Scientific World Journal
author_facet Gertrud K. Nürnberg
author_sort Gertrud K. Nürnberg
title Quantified Hypoxia and Anoxia in Lakes and Reservoirs
title_short Quantified Hypoxia and Anoxia in Lakes and Reservoirs
title_full Quantified Hypoxia and Anoxia in Lakes and Reservoirs
title_fullStr Quantified Hypoxia and Anoxia in Lakes and Reservoirs
title_full_unstemmed Quantified Hypoxia and Anoxia in Lakes and Reservoirs
title_sort quantified hypoxia and anoxia in lakes and reservoirs
publisher Hindawi Limited
series The Scientific World Journal
issn 1537-744X
publishDate 2004-01-01
description Hypoxia and anoxia occur frequently in freshwater systems and have biological and chemical implications. Anoxia can be expressed and quantified as the anoxic factor; hypoxia, for a specific level of oxygen depletion, can be expressed as the hypoxic factor in lakes, reservoirs, and river sections. These methods summarize information of individual dissolved oxygen profiles as annual values or factors that facilitate comparison between and within lakes. Therefore, these factors are useful in the formulation and testing of hypotheses related to the dissolved oxygen status in water bodies. Methods of calculating different factors for different oxygen levels and water layers, including those applying separately to the epilimnion and hypolimnion, are presented in detail. Proven and potential applicability include: (1) the quantification of relationships with lake water quality variables and lake classification (trophic state), (2) the evaluation of restoration techniques with respect to their effects on hypolimnetic oxygen depletion, (3) the determination of internal phosphorus loading in stratified and polymictic lakes, (4) the exploration of habitat constraints due to hypoxia (e.g., fish species richness and winterkill), (5) forecasting potential effects of climatic change on oxygen content and internal phosphorus loading, and (6) the establishment and examination of criteria and guidelines with respect to hypoxia by custom-made definitions.
url http://dx.doi.org/10.1100/tsw.2004.5
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