<a href=showthread.php?s=&postid=12405563#post12405563 target=_blank>Originally posted</a> by Reefun
So basically my two questions are:
1. How could my dkh keep going down while calcium remained relatively unchanged?
The most likely answer, if the result were “real†(see what I mean below) would be the addition of an acid. An acid will reduce alkalinity without necessarily affecting calcium.
In order to measure a change in concentration of something in sea water (e.g., calcium concentration, magnesium concentration, total alkalinity) we have observe a change in concentration larger than the error of our analytical method.
For example, the accuracy with which we can measure calcium concentration in sea water is about +/- 5%, which really isn’t too bad for a hobbyist grade test kit. Since the calcium concentration in NSW is ~412 ppm we can measure the concentration accurately to within about +/- 20 ppm. In other words, if the calcium concentration changes by less than ~20 ppm, we cannot accurately or confidently measure a change in concentration. This also means that if we measure a concentration of 400 ppm, the real concentration should be within roughly the range of 380-420 ppm, but we cannot determine where it is in that range without using a more accurate analytical method.
For total alkalinity we see the same sorts of concerns. We can measure alk. to within a margin of error, but we can’t determine where in that margin of error the real value isâ€"we can just shrink the error by using better methodology. For alk. measurements we can typically see an error of about +/- 1 dKH (or about +/- 0.35 meq/l). So, if we measure 9 dKH, the real value is likely somewhere in the range of 8-10 dKH. If the alk. changes more than 1 dKH we can measure a change in total alkalinity, but we cannot accurately measure a change if the change is not at least that large.
When calcium is removed from the water to build skeletons, two equivalents of alkalinity are also removed:
Ca2+ + 2HCO3- = CaCO3 + CO2
This reaction proceeds as a molar ratio, not as a mass ratio. We normally measure calcium based on mass (ppm calcium is equivalent to grams of calcium per kilogram of SW). If you do the calculation you find that for every 1 meq/l = 2.8 dKH of total alkalinity you remove from the water you also remove 20 ppm calcium.
Recall, we have to remove a MINIMUM of 20 ppm calcium just to be able to accurately measure any change at all. In order to achieve this change in calcium we have removed roughly 3x the amount of alkalinity we need to in order to see a change in concentration.
Imagine, for example, that you measure a drop in alk. of 1 dKH in your aquarium after a couple of days. That is a big enough change to say with confidence that the alk. has fallen by about 1 dKH. How much should the calcium have changed? The calculation is fairly simple: 20/2.8 ~ 7 ppm. That change in calcium is too small to measure, meaning that we would get about the same measured value for calcium. This could give us the impression that alkalinity is falling while calcium is remaining stable, however, this is an artifact that results simply due to the nature of measuring these parameters in SW. There is almost 5 times as much calcium in NSW as there is alkalinity. We can easily measure a 10% change in calcium concentration or total alkalinity in your sea water, but a 10% reduction of alkalinity causes less than a 2% change in calcium due to the difference in background concentration.
The most likely scenario is that both are decreasing, but due to the nature analytical chemistry and statistics, you can only measure that change that is occurring in both by measuring alkalinity.
<a href=showthread.php?s=&postid=12405563#post12405563 target=_blank>Originally posted</a> by Reefun
2. How did my magnesium level get to where it is now? Nothing was ever added to the tank other than the Kent products mentioned and Kent turbo calcium in very small amounts.
Tank is just over two months old and only in the last month had anything in it that would use calcium
No idea…more info please.
Chris