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Hanna checker getting DinosHow are you testing, what’s in the tank, do you need po4 because corals are suffering? ….you just want a po4 reading on a hobby test kit, so dose more!
Already dose 2 bottles of neophoseCalcium carbonate surfaces can bind a lot of phosphate from the water column. You may just need to continue dosing more phosphate to the tank.
maybe is not strong enoughYou get dinoflagellate because it’s a new tank, not zero po4….don’t believe the propaganda!Hanna checker getting Dinos
I've never used that product so I'm not sure. It might be cheaper to mix your own solution using some trisodium phosphate.Already dose 2 bottles of neophosemaybe is not strong enough
I was only talking about calcium carbonate surfaces like live rock or sand binding phosphate. I believe dissolved calcium in the water behaves differently due to other dissolved ions that prevent precipitation in saltwater but I lack the chemistry background to fully understand this relationship.As someone else mentioned, it readily binds to calcium. This is why it’s problematic, because it can make the calcium that corals need to build their skeletons unavailable because it’s bound up with phosphate.
My understanding (as a non-chemist) is that it can bind to calcium in the water if conditions are right, and precipitate out as calcium phosphate. Drops in pH can break apart that bond, releasing phosphate (and calcium) back into the water. Some bacteria do this too, consuming the phosphate and leaving behind calcium, but both are likely to be a slow process in a typical reef rank.I was only talking about calcium carbonate surfaces like live rock or sand binding phosphate. I believe dissolved calcium in the water behaves differently due to other dissolved ions that prevent precipitation in saltwater but I lack the chemistry background to fully understand this relationship.As someone else mentioned, it readily binds to calcium. This is why it’s problematic, because it can make the calcium that corals need to build their skeletons unavailable because it’s bound up with phosphate.
As someone else mentioned, it readily binds to calcium. This is why it’s problematic, because it can make the calcium that corals need to build their skeletons unavailable because it’s bound up with phosphate.
For that reason, be very careful with soaking. You might see no change at all until you hit saturation point and then it’ll skyrocket. Make sure you’re using a sensitive tester like Hanna ULR once you get it dialed in, but you can use cheaper tests and test more frequently until then.
My understanding (as a non-chemist) is that it can bind to calcium in the water if conditions are right, and precipitate out as calcium phosphate. Drops in pH can break apart that bond, releasing phosphate (and calcium) back into the water. Some bacteria do this too, consuming the phosphate and leaving behind calcium, but both are likely to be a slow process in a typical reef rank.
This is also another benefit of “cured” live rock—the phosphate has already been bound up to the rock, meaning increased stability over the first few weeks to months versus dry rock.
Hopefully someone will correct me if my basic understanding is wrong, and I know I’m oversimplifying.
I can’t remember where I saw it (maybe a BRS video?) but there was some testing where they saw a pattern of phosphate suddenly jumping after a certain point. I’ll see if I can find it again, but either way do you happen to know what the mechanism would be that causes this?As someone else mentioned, it readily binds to calcium. This is why it’s problematic, because it can make the calcium that corals need to build their skeletons unavailable because it’s bound up with phosphate.
For that reason, be very careful with soaking. You might see no change at all until you hit saturation point and then it’ll skyrocket. Make sure you’re using a sensitive tester like Hanna ULR once you get it dialed in, but you can use cheaper tests and test more frequently until then.
I don’t think that’s the rationale for whatever impact phosphate has on calcification.
There also is not a sudden saturation point. The higher phosphate goes, the more
Binds.
I can’t remember where I saw it (maybe a BRS video?) but there was some testing where they saw a pattern of phosphate suddenly jumping after a certain point. I’ll see if I can find it again, but either way do you happen to know what the mechanism would be that causes this?