Siesta, reduced surface movement etc, will not do this, to get the level for serious PR in aquatic polanted systems, you need: A LOT oif light(eg, the sun), a weed choked cess pool, say a lake packed with Hydrilla(common in Florida), and then you start getting O2 levels in 150-200 % range, we rarely even get beyond 110-130%.
If you reduce water flow, then less CO2 will get to the plants and less nutrients etc, in a densely planted water column.
Denser than anything we might want, but a few neglected tanks might illustrate.
I think you are correct about CO2 helping to address PR with O2 super saturation above AMBIENT O2.
In that case, the more CO2, the less competition for O2 at RUBISCO's active site.
If you reduce one, say CO2 a great deal, then O2 is more likely to enter. If you increase CO2 and reduce O2, then the opposite.
If you increase the concentration of both of them, then the relative amounts should fairly equal if the concentrations are the same.
So if you add say 2x the O2, say go from 7ppm to 14ppm, then added say 7ppm then up to 14ppm........., we should see somewhat similar effects.........since the ratio of molecules coming into contact with RUBISCO are relatively the same, but at higher levels.
O2 is a rather toxic however and the radicals of O2 can cause issues. This occurs when photosynthesis is really driven very hard, too fast for the cells to respond or when something breaks down in the cellular machinery.
But for our case with CO2 enrichment, we are adding roughly 10-20X ambient levels of CO2 and then also only getting near 120% in a well run tank.
I'd say that's better than 3ppm or less and 100% O2 like in a non CO2 tank.
The ratio is much different there.
Here's Bowes' paper of CO2 and O2:
http://sesultan.web.wesleyan.edu/wes...nce_carbon.pdf
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