I am DO levels in stagnant waters from a stream mesocosm experiment. During the non-flow periods, DO saturation measurements are reaching maximums of 300% (26 mg/L, 21 degrees C). The flumes contained high amounts of filamentous algae and high light inputs, which might partially explain these values. Nevertheless, we are afraid that oxygen bubbles might be generating an artefact.

We are wondering which are the maximums levels recorded by other researchers in similar conditions?

Thanks all for your help and time,

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