Hi Hermit,
Thanks for the info, and the warm welcome. It is a shame that all the kalkwasswer boards are not condensed into one, as I already posted a similar message/question in another.
My confusion is based on this "buffering" effect of kalkwasser. Why is it considered a buffering agent rather than something to increase Ca with? From the limited chemistry I know (I am a geophysics major: earthquakes, plate tectonics, and the like), lime will revert to Ca and OH ions when mixed with water. The OH ions raise the pH of the water. When you then put the lime water in the reef tank, you increase the number of Ca and OH ions in the tank. You mention that phosphates are precipitated out during this process. To me, this means that some of the free Ca is bonding with phosphates. However, if there are not many phosphate ions in the tank, there will be a surplus of Ca ions in the end. Therefore, you now have raised the Ca of the tank, and produced a good Ca buffer. As for the OH, if everything is simple, you have now increased the pH of the tank.
So can anyone add to this, or correct me if I'm wrong? I am just trying to gain confidence in myself by understanding the system before I go buying corals for my tank.
thanks,
sam