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Lakes and Watercourses

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Oxygen status <strong>and</strong><br />

oxygen-consuming<br />

substances<br />

Introduction<br />

Dissolved oxygen is vital for respiration <strong>and</strong> many microbial <strong>and</strong> chemical<br />

processes in the ecosystem. The concentration may thus regulate the<br />

biological structure. Oxygen conditions vary, mainly due to changing<br />

production conditions <strong>and</strong> the organic load, including natural humic<br />

substances leaching from the catchment area. In the bottom water of<br />

stratified lakes (the hypolimnion), the oxygen situation is at its worst at<br />

the end of the stagnation period in summer, at which time conditions<br />

may become critical for many organisms. The end of the period when<br />

lakes <strong>and</strong> rivers are ice-covered is another crucial time. Oxygen conditions<br />

in watercourses may be poorest at times of low flow, particularly in<br />

polluted rivers. Significant variations in oxygen levels <strong>and</strong> oxygen<br />

saturation can occur from one day to the next in the surface waters of<br />

unstratified lakes <strong>and</strong> in rivers <strong>and</strong> streams.<br />

Oxygen concentration is prefered to saturation as a means of characterising<br />

oxygen status because the thresholds of tolerance of various<br />

organisms are usually expressed as concentrations. However, merely<br />

stating the oxygen concentration may give an incomplete picture of<br />

oxygen conditions, particularly in rivers <strong>and</strong> streams. This is due to<br />

variations in oxygen input <strong>and</strong> organic load. The presence of oxygenconsuming<br />

substances should therefore also be taken into account. The<br />

concentration of organic matter provides essential information about the<br />

risk of low oxygen levels occurring between the occasions on which<br />

oxygen concentrations are monitored.<br />

A high oxygen concentration or oxygen saturation is not always a sign<br />

of a ”healthy” environment. Assimilation by plants may result in saturation<br />

figures of over 100 per cent in eutrophic waters.<br />

Scales have only been given for assessing current conditions because<br />

of the difficulties of determining reference values.<br />

Assessment of current conditions<br />

Oxygen status is assessed in the bottom waters of stratified lakes <strong>and</strong> also<br />

in the circulating water column in unstratified lakes. Annual minimum<br />

values based on concentrations monitored during critical periods (late<br />

29

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