antonsemrad
New member
Does the added CO2 in the worlds oceans affect alkilinity? If so, how? If not, what has been the alkilinity of NSW historically speaking? (has it changed)
Thanks
Anton
Thanks
Anton
Ok, I am under the impression that average reef alkalinity is around 2.5 meq/l. I do however prefer to run my tank at 3.5 meq/l.
According to randy's article "what is alkalinity"
Well, the carbonic acid can release protons by reversing equations 1 and 2:
(5) H2CO3 ==> H+ + HCO3-
(6) HCO3- ==> H+ + CO3--
These protons can go on to reduce alkalinity by combining with something that is in the sample that provides alkalinity (carbonate, bicarbonate, borate, phosphate, etc). However, for every proton that leaves the carbonic acid and reduces alkalinity, a new bicarbonate or carbonate ion is formed that adds to alkalinity, and the net change in total alkalinity is exactly zero. The pH will change, and the speciation of the things contributing to alkalinity will change, but not the total alkalinity.
I can add CO2, sodium carbonate or sodium bicarbonate to my tank and increase alkalinity. If I mix the carbonate and bicarbonate in the right proportions, my solution can equal the tank pH. If I then pour that same pH solution in the tank, I won't change pH but will increase alkalinity. OTOH, if I added carbonate (i.e. washing soda...am ignoring the sodium since it dissociates into the huge Na pool), the pH of a solution is around 11, so the pH and the alkalinity of the tank water goes up. The pH, in turn, shifts the equations below towards carbonate in the tank.
I can add CO2, sodium carbonate or sodium bicarbonate to my tank and increase alkalinity. If I mix the carbonate and bicarbonate in the right proportions, my solution can equal the tank pH. If I then pour that same pH solution in the tank, I won't change pH but will increase alkalinity. OTOH, if I added carbonate (i.e. washing soda...am ignoring the sodium since it dissociates into the huge Na pool), the pH of a solution is around 11, so the pH and the alkalinity of the tank water goes up. The pH, in turn, shifts the equations below towards carbonate in the tank.
What Randy is saying is that in a given volume of water with a given alkalinity, if you shift pH, you change from CO2 at low pH to CO3 at high pH.
Kalkwasser is calcium plus some hydroxides. The hydroxides raise pH and move CO2 in air and water towards carbonate. So, in this case, the OH, while containing no C, creates alkainity from CO2 when in solution (hence the CaCO3 crust that forms on the surface of kalkwasser solution).
And yes, it appears that the primary acidification of the ocean is the reason for the loss of carbonates. And this is where the terminology gets tricky, because at normal oceanic pH's, you have to see which species predominates. Near anoxic muds in mangroves..or in freshwater...you can calcify but the calcium carbonate dissolves. That's what is happening in the world oceans...decreased calcification and increased carbonate dissolution, but the latter is on longer time scales, so the release of dissolved carbonates does not balance the rate of acidification by CO2 input.
before the industrial revolution huh.... you may want to look at the recent upward temp swing that all of the global warming nuts keep talking about... most of it came before the industrial revolution also