Phosphate binds to aragonite in a reversible bind to the equilibrium in the outside water. If new calcium carbonate grows over the old structure, then the phosphate is locked in until the structure is "melted."
Aragonite can bind large amounts of phosphate many, many times more than in the water column. Dr. Holmes-Farley says that it binds in an exponential fashion where it will bind more with higher concentrations in the water.
Even in my tank with .01 phosphate, if we soaked some of the sand in a small volume of fresh saltwater, it would read out with quite a high number.
Most of the time, the aragonite binds this stuff once it is dead and not so much while it is living. I have tested fresh acro skeletons and they release very little phosphate, even in small concentrations of water. I also tested some large-size ARM and they had just a trace of phosphate in 1l of water at 15 ppb (0.000068 ppm in a 180G tank).
Aragonite can bind large amounts of phosphate many, many times more than in the water column. Dr. Holmes-Farley says that it binds in an exponential fashion where it will bind more with higher concentrations in the water.
Even in my tank with .01 phosphate, if we soaked some of the sand in a small volume of fresh saltwater, it would read out with quite a high number.
Most of the time, the aragonite binds this stuff once it is dead and not so much while it is living. I have tested fresh acro skeletons and they release very little phosphate, even in small concentrations of water. I also tested some large-size ARM and they had just a trace of phosphate in 1l of water at 15 ppb (0.000068 ppm in a 180G tank).

But yes, there's much more experimenting and testing to be done about these parameters!

