@Lasse manages his cyanobacteria growth with phosphate and nitrate additions. The thinking is that raising the concentration of these nutrients encourages microorganism growth and competition for cyanobacteria.
I must have been bad in explaining my thoughts. I do not see it primary as a competition for nutrients in the water.
My theory in short
According to mat building cyanobacteria - they are always present but not always form mats. I think that the critical point is when they decide to build mats or with other words take some of the energy from the photosynthesis and excrete a slime of mostly carbohydrates. My idea is that when they can catch PO
4 from the water column - they do that and they have some competition some algae and fungus about available space. They stay put. If the PO
4 will be sparse or nonexistent - they need to get PO
4 from other sources. On way of doing this is to form a mat that create anaerobic environment between the mat and substrate. In this anaerobic environment bacteria will grow - both Nitrogen fixating bacteria, denitrifikation bacteria and when the NO
3 is zero or very low - bacteria that produce hydrogen sulphide will establish themselves. The hydrogen sulphide will break the bounds between different metals and phosphate in the substrate and phosphate will be released to the hungry cyanobacteria. If the area they establish themself content a high amount of organic matter - PO
4 will be released from the organic matter too. When the trigger had started the mat forming - it becomes a self playing piano between the mat and the substrate - first when all P has gone - the mat start to decline.
According to nitrate - I not only concentrate me on that because it is a inorganic nitrogen source - there is plenty of other sources of inorganic N and even some organic N (amino acids) that unicellular organism can use both in a autotrophic and an heterotopic way (primary and secondary producers). I´m interested of NO
3 because it has another important role in anaerobic bacterial community. As long NO
3 exist in the water - it block most of the hydrogen sulphide producers, hence the release of PO
4 from metal-PO
4 compounds in the substrate.
I do believe that low PO
4 can be a trigger for mat forming but also low NO
3 can act that way too. Probably there is other triggers too. I also believe that there can be part of the tank there it can microenvironment with low PO
4 or NO
3 - especially in tanks with low flow or dead spots.
Because I see the mat forming as the Gordian knot - I use three actions when the mats has establish themselves. Disturb the mats as much as possible, have enough high NO
3 levels in order to have zero hydrogen sulphide production below the mats and if PO4 is low - have a PO4 concentration between 0.05 to 0.1 mg/L. Good circulation (I love standing waves) in order to not establish favorable microenvironment can help too
I agree that this is only a theory and do not need to be the truth. However - the theory have helped me to stand free from Cyanobacteria mat forming for most of the time and with a treatment schema when things goes downhill. The schema include disturbing of the mats, keep up PO
4 to 0.05 - 0.1, rise the NO
3 up to at least 5 ppm and sometimes go down in light intensity and slowly rise it back to normal during a couple of weeks. The lowering of the light aim to lower the secret (slime) production (they need photosynthesis for that).
I prefer to work with the biology instead of nuking it.
Sincerely Lasse