Boy is this thread a can of worms
Why folks do it, I am not sure? perhaps they we told? not sure
As people "think", more means better = more growth and I have always said no and recent data says so.
balance plays a role but it doesnt stop the fact that calcium stops a coral from growing
Where did this come from
Coral grow is at pretty much the same rate from 360 ppm to 500 ppm Ca++. The issue is high Ca++ is not needed. It is more on the Ca/Mg ratio, its Alk and pH. When one sees coral growth or coral growth reduction it is NOT just a Ca++ issue, it is a set of multi-complex issue, as a function of coral biology and solution /coral chemistry kinetics.
Well we no the MG has an effect of alk right, it binds it and does not allow the alk to attach the calcium ion and then precipitate out of solution. So if we ran high levels of MG what would the effect be with i the coral and thus its ability to grow??
Low Mg++, increases abiotic precip of CaCO3 which is not the same thing as biotic to a degree but see below. Normal levels of Mg++ act as a protective inhibitor for abitoic precip of CaCO3 as it "poisons" the surface slowing down CaCO3 precip. This is not a coral.
Mg++ has about nothing to do with coral growth /say for us. It is just a substitute ion for Ca++, as it is there in seawater, just as Sr is, which substitutes for Ca++ in Aragonite. Furthermore, Mg++ does not fit into a Aragonite crystal lattice. However, in most hard colors there, is some Hi-Mg++ Calcite and even Lo-Mg Calcite growth sites within the the coral skeleton along with the mostly Aragonite skeleton.
Maybe me needs to bring my adopted son here Chis Jury to explain all, as his field is coal growth biology and its kinetics as a function of Ca++, Mg++, pH and Alk. Some things he has mentioned in a question on this subject of Mg++.
Above a molar Mg/Ca ratio of ~2 in sea water we have an aragonite nucleation field for abiotic precipitates. Hi-Mg calcite can also form though. A ratio of 1-2 favors hi-Mg calcite, while ~1 or less yields a low-Mg calcite nucleation field (again, for abiotic precipitates). Organisms can deviate from that a bit, but their calcification is influenced by variation in seawater chemistry (some more, some less). Ries has done some really spectacular work on this in the last several years. I've uploaded two of those papers (Ries, 2004; Ries et al., 2006) to the PDF library. Ries et al., (2006) is the one most applicable here, but some methods are referenced that are explained in Ries (2004).
I'm going to guesstimate that the Ca++ concentration is probably somewhere in the neighborhood of 400-500 ppm. With a molecular weight of 40.08, that means 9.98-12.48 mmol/kg Ca++. Mg++ has a molecular weight of 24.30, so that's 28.8 mmol/kg Mg++. For 400 ppm Ca++ we have a Mg/Ca ratio of 2.89. For 500 ppm Ca++ we have a Mg/Ca ratio of 2.31.
Ries et al., (2006) tested the effects of a Mg/Ca ratio of 1.0, 1.5, 2.5, 3.5, and 5.2--spanning the range from the Cretaceous to today's sea water. To make the ratios go down ionic strength was held constant while calcium concentration was increased and magnesium reduced so as to achieve the desired ratio (Ries, 2004). They used 3 coral species: Acropora cervicornis, Montipora digitata, and Porites cylindrica. As the Mg/Ca ratio dropped from modern to ancient chemistries all the corals started to produce a mixture of aragonite and calcite, and the Mg content of the calcite was proportional to that in the sea water. At the lowest Mg/Ca ratio of 1.0 the corals were all producing ~1/3 of their skeletons as low-Mg calcite.
They also measured rates of calcification. The M. digitata actually performed best in the Mg/Ca ratio of 3.5 with 2.5 coming in second. They grew slowest in 'modern' sea water (5.2), 'Cretaceous' sea water (1.0) and 'early Cenozoic' sea water (1.5), though I wonder if at least the decrease in modern sea water might be related to the absolute Ca++ concentration more than the Mg/Ca ratio. In any event, the other two corals (A. cervicornis and P. cylindrica) both grew equally well with a 5.2 and 3.5 ratio. P. cylindrica did well in 2.5 as well, but A. cervicornis dropped off quite a bit. Neither A. cervicornis nor P. cylindrica did particularly well in the 1.5 and 1.0 Mg/Ca ratios.
As above, I don't think the 2.3-2.9 ratio that we probably have here is enough to reduce calcification for the Montipora, but it could be, or it could be getting pretty close. It may well be enough to reduce calcification for some corals though. Most likely this reduction has something to do with reduced ability to induce nucleation of the preferred polymorph by the corals (i.e., they're somehow equipped to produce aragonite and calcite crystals keep nucleating), but who really knows at this point?
All please read this thread. It is really the pH and Alk that is "the" thing kinda. In short, if one keeps All at or near NSW and just increases the Alk there will/may be better coral growth and some studies have show this.
Chris Jury/MCsaxmaster article on calcification! - Reef Central Online Community