Hi folks,
I am into the science part of this hobby and I have been experimenting with setting up a phytoplankton refugium for years now. I grow phytoplankton in a refugium, in the same water as the main display. I works, sort of, but particularly long term stability is hard. For example, now I have problems getting good growth in water that has been reused for 10 weeks, no matter how much fertilizer I add. The water has been filtered well with GAC, and a bit of ozone, along the way. Right now I am investigating if the EDTA in the Guillard F/2 fertilizer I am using is causing issues. In total I have now added at least 4 times the amount of F/2 fertilizer that it would take to get the whole water volume to F/2 concentration.
Is it so that EDTA stays in the water even after the metal it was chelated to is taken up? Can it potentially chelate a new ion, recycling itself? Is it stable so that it is only removed very slowly by GAC, ozone and biological processes? Could it make life gradually harder (as the concentration rises) for microorganisms when it comes to taking up metals? At the moment the potential concentration could be more than 50 micromol per liter, if nothing has been lost.
I am into the science part of this hobby and I have been experimenting with setting up a phytoplankton refugium for years now. I grow phytoplankton in a refugium, in the same water as the main display. I works, sort of, but particularly long term stability is hard. For example, now I have problems getting good growth in water that has been reused for 10 weeks, no matter how much fertilizer I add. The water has been filtered well with GAC, and a bit of ozone, along the way. Right now I am investigating if the EDTA in the Guillard F/2 fertilizer I am using is causing issues. In total I have now added at least 4 times the amount of F/2 fertilizer that it would take to get the whole water volume to F/2 concentration.
Is it so that EDTA stays in the water even after the metal it was chelated to is taken up? Can it potentially chelate a new ion, recycling itself? Is it stable so that it is only removed very slowly by GAC, ozone and biological processes? Could it make life gradually harder (as the concentration rises) for microorganisms when it comes to taking up metals? At the moment the potential concentration could be more than 50 micromol per liter, if nothing has been lost.


