So I just made the mistake of overdosing too much kalk slurry in one go and caused alk and [Ca] to drop a lot. Theres tonnes of other reefers who've posted about making the same mistake, and thanks to them and their advice I've been able to minimize the damage by dosing vinegar.
However, one thing that I do not seem to understand is why dosing kalk over a short vs long period of time should make a difference, at least assuming basic chemical theory. If one doses x amount of kalk, Ca(OH)2, the total amount of Ca2+ and OH- ions being added are the same if I dose this in one night vs over a week. Since the equilibrium constants theoretically do not change, I should see the same amount of precipitation if I did this over one week. Even with coupled equilibria, the constants are multiplicative so the final equilibrium concentrations shouldn't have a "path-dependence" through time. Further, this theory does not predict why adding a Ca containing compound would cause resulting [Ca] to be lower than started with (unless this is temporary).
Is there an accepted explanation to this or is this something that we do not know about yet? I know there are models like MIAMI which are used in academia. Do these models predict this behaviour? My only hypotheses are that the equilibrium constants change fast enough when extremely high [OH-] in one spot causes calcium to precipitate in a way that they become catalysts for more precipitation in a runaway reaction, or that somehow the precipitated calcium and alkalinity physically become unavailable to undergo the reverse reaction. Do people know if this only happens in reef tanks, or in newly made fresh seawater as well? How does temperature play into this?
However, one thing that I do not seem to understand is why dosing kalk over a short vs long period of time should make a difference, at least assuming basic chemical theory. If one doses x amount of kalk, Ca(OH)2, the total amount of Ca2+ and OH- ions being added are the same if I dose this in one night vs over a week. Since the equilibrium constants theoretically do not change, I should see the same amount of precipitation if I did this over one week. Even with coupled equilibria, the constants are multiplicative so the final equilibrium concentrations shouldn't have a "path-dependence" through time. Further, this theory does not predict why adding a Ca containing compound would cause resulting [Ca] to be lower than started with (unless this is temporary).
Is there an accepted explanation to this or is this something that we do not know about yet? I know there are models like MIAMI which are used in academia. Do these models predict this behaviour? My only hypotheses are that the equilibrium constants change fast enough when extremely high [OH-] in one spot causes calcium to precipitate in a way that they become catalysts for more precipitation in a runaway reaction, or that somehow the precipitated calcium and alkalinity physically become unavailable to undergo the reverse reaction. Do people know if this only happens in reef tanks, or in newly made fresh seawater as well? How does temperature play into this?