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Hello, maybe this question is mostly adressed to Randy, so I would be very happy for his explanation, but other as well who knows. I have an own theory but before I establish that I must get this checked by a PRO like our Randy.
If we take the effluent water from the calciumreactor, we have around 45dKH and 740 ppm Ca in that water. The reason of no spontaneous precipitation of that is the low pH, which due two the CO2 content of that effluent water is maybe around 6.5. Well, at least so low so there exist no CO3-ions, and then the saturation index (CaxCO3) is far below the point when it forces CaCO3 spontaneously. The saturation index due to phosphate/Mg etc have to be at least above 5 to precipitate as far as I have understood, and with a pH of 6.5 we have such low CO3 (close to 0) so the sat.index is too low to accomplish CaCO3-formation.
But: If I now take this water from the calcium-reactor and aerate it, so the CO2 is degassing and pH rises to around 8.2, well, then we all know that the total alkalinity is the same (around 45dKH) and of course also the Calcium (around 740ppm). Why does this solution not precipitate to CaCO3 with a pH of 8.2, dKH of 45 and Calcium of 720?. We know empirically that it does not.
My question here is if my theory is correct:
When degassing the excess of CO2, so we reach the pH 8.2 we of course have the same total alkalinity, but we got an alteration in the composition of the total alkalinity so there will be less carbonates and more borates(and other ions) which build up this 45dKH alkalinity. That is not my question, that I know is the case. But is that also the reason why it is not precipitating? That is my question, is the cause of no precipitation in this scenario due to that we loose so much Carbonate-alkalinity during the degassing of Co2, and proportional increase the more borate-alkalinity (and other ions) so we get no saturation index above around 5?. Then it should by the way be very contraproductive to degassing the water from the calciumreactor too much, at least to the pH of 8.2.
Thoughts and response please
Jonas Roman
If we take the effluent water from the calciumreactor, we have around 45dKH and 740 ppm Ca in that water. The reason of no spontaneous precipitation of that is the low pH, which due two the CO2 content of that effluent water is maybe around 6.5. Well, at least so low so there exist no CO3-ions, and then the saturation index (CaxCO3) is far below the point when it forces CaCO3 spontaneously. The saturation index due to phosphate/Mg etc have to be at least above 5 to precipitate as far as I have understood, and with a pH of 6.5 we have such low CO3 (close to 0) so the sat.index is too low to accomplish CaCO3-formation.
But: If I now take this water from the calcium-reactor and aerate it, so the CO2 is degassing and pH rises to around 8.2, well, then we all know that the total alkalinity is the same (around 45dKH) and of course also the Calcium (around 740ppm). Why does this solution not precipitate to CaCO3 with a pH of 8.2, dKH of 45 and Calcium of 720?. We know empirically that it does not.
My question here is if my theory is correct:
When degassing the excess of CO2, so we reach the pH 8.2 we of course have the same total alkalinity, but we got an alteration in the composition of the total alkalinity so there will be less carbonates and more borates(and other ions) which build up this 45dKH alkalinity. That is not my question, that I know is the case. But is that also the reason why it is not precipitating? That is my question, is the cause of no precipitation in this scenario due to that we loose so much Carbonate-alkalinity during the degassing of Co2, and proportional increase the more borate-alkalinity (and other ions) so we get no saturation index above around 5?. Then it should by the way be very contraproductive to degassing the water from the calciumreactor too much, at least to the pH of 8.2.
Thoughts and response please
Jonas Roman






