Hi Randy,
In my tank I am going to use a dry rock called Pukani. It is the calcium carbonate coral skeletons mined from a dead coral reef no longer submerged in the ocean. It is also claimed to leach phosphates into the tank for quite some time (even years).
One group of folks, including BRS that sells Pukani, are adamant the phosphate comes from breakdown of organic material hidden in the unseen inner cavities of the rock - NOT from the rock itself.
Others feel phosphate it is being released from the rock and they soak it in acid which they claim eats away at the outer skin of the rock (where the phosphates are bound).
I have been curing my Pukani in large saltwater bins in the garage for over 2 months and I still see phosphate levels build back up after each 100% water change (although it seems to be diminishing over time).
I was originally thinking it was due to organic breakdown but after reading your article Phosphate In The Reef Aquarium: By Randy Holmes-Farley I am beginning to wonder if perhaps both groups are right and that it might be a combination?
In your article, you talked about the binding of phosphate to calcium carbonate surfaces in a higher pH environment (maximized at around pH 8.4) and how both aragonite sand and coral “skeletons” can act as a sink/reservoir for phosphate (assuming the pH remains at these higher levels). This allows algae to thrive despite cutting off all other external sources of phosphate.
I assume you mean the algae is feeding off this phosphate and if so, how is it released given the same higher pH environment maintained in most reef tanks?
Does pH play a significant factor here in terms of phosphate binding/releasing and if so, at what levels would we expect to see it shift one way or the other?
In my tank I am going to use a dry rock called Pukani. It is the calcium carbonate coral skeletons mined from a dead coral reef no longer submerged in the ocean. It is also claimed to leach phosphates into the tank for quite some time (even years).
One group of folks, including BRS that sells Pukani, are adamant the phosphate comes from breakdown of organic material hidden in the unseen inner cavities of the rock - NOT from the rock itself.
Others feel phosphate it is being released from the rock and they soak it in acid which they claim eats away at the outer skin of the rock (where the phosphates are bound).
I have been curing my Pukani in large saltwater bins in the garage for over 2 months and I still see phosphate levels build back up after each 100% water change (although it seems to be diminishing over time).
I was originally thinking it was due to organic breakdown but after reading your article Phosphate In The Reef Aquarium: By Randy Holmes-Farley I am beginning to wonder if perhaps both groups are right and that it might be a combination?
In your article, you talked about the binding of phosphate to calcium carbonate surfaces in a higher pH environment (maximized at around pH 8.4) and how both aragonite sand and coral “skeletons” can act as a sink/reservoir for phosphate (assuming the pH remains at these higher levels). This allows algae to thrive despite cutting off all other external sources of phosphate.
I assume you mean the algae is feeding off this phosphate and if so, how is it released given the same higher pH environment maintained in most reef tanks?
Does pH play a significant factor here in terms of phosphate binding/releasing and if so, at what levels would we expect to see it shift one way or the other?



