George Farmer said:
ceg4048 said:
Pressure and temperature are by far the most important factors in the dissolution rate of any gas in any liquid
Does that mean with cooler water less CO2 injection is required to reach a given level compared with warmer water?
Hi George,
Yes this is correct! Check out the chart shown below:
(Chart courtesy of engineeringtoolbox.com)

This chart shows the solubility of CO2 as a function of temperature. On the vertical axis this indicates how many grams of CO2 will dissolve in 1Kg of water at 1 atmosphere of pressure.
At about 24 deg.C the solubility is about 1.5 grams per Kg of water.
At about 30 deg.C the solubility is about 1.25 grams per Kg of water.
So just lowering the water temperature by 6 degrees increases the solubility of this gas by 20%.
However, the solubility of the gas also is a function of the pressure. That function is Henry's Law which states that under constant temperature:
Gas Pressure = (Solubility constant)*(Concentration) or P=k*C
This is a simple ratio and if you solve the equation for the constant k => P/C then this means that the ratio of a gases pressure to it's concentration is constant. So if you increase the pressure by 20% then the solubility immediately increases by 20%.
What does this all mean? It means in relation to your question that all you have to do in a warmer tank is to tweak the needle valve slightly and you can immediately compensate for the loss of solubility due to increases temperature by simply increasing the injection pressure. So if I had excellent CO2 at 24 degrees with my needle valve set to 1.5 psi and then I got discus and had to increase my tank temperature to 30 degrees, then I just need ti increase my needle valve setting by 20% i.e. 0.3 psi to make the new working pressure 1.8 psi. That keeps the solubility of the gas about the same.
George Farmer said:
This is interesting, as I also assume a plant's nutrient requirement goes up as temperature increases due to the increase in metabolic processes?
Yes this is true, but that then means you must increase the CO2 even more than just compensating for the solubility decrease due to increased consumption requirements.
Tom said:
I'm simply trying to go through each possibility changing one thing at a time, seeing if there is any difference. Trial and error. It was just my thought that if the water was jam packed with loads of solids, it might be harder to dissolve something into than if it had a very low TDS
Actually, the only solid dissolved in water that has a serious impact on CO2 solubility is salt, NaCl. That's why CO2 is less soluble in ocean water than in fresh water.
Tom said:
It's not as if the CO2 has been all over the place in terms of stability either (just increasing every so often), so in that case the only option is more
Well, if we're seeing BBA then the tank is disagreeing with you, right? Because BBA is only ever causes by poor/unstable CO2. Even if it were true that higher TDS caused lower gas solubility, then that would only mean that you should get a low CO2 algae, like hair, not a fluctuating CO2 type algae, because the solubility although lower, would still be constant.
The focus here I reckon is to determine what mechanism is causing the instability. A dropchecker won't always show you instability because it's response time is so slow.
Is it possible that your regulator is allowing surging? Do you have another that you could try? Is the dropchecker yellow at the time of lights on? Have you measure the pH profile throughout the photoperiod in order to plot pH v time? I think you need to do this to absolutely determine if there is an instability.
The species in your old tank all appear to be those having a lower CO2 compensation point. Are there the same species in your new tank?
BBA also is a tenacious species, so that even if you fix the conditions it won't just go away. Have you tried blackout and/or Excel overdose to eliminate it from the tank completely?
Just some ideas to kick around...
Cheers,