Hi Elliott & Tom - that last paragraph represents my immediate hesitation re the polluted vile possibility; however I do realize that it's just a single possibility of probably several others.
I didn't have much time yesterday to get online, but I did pop into my subject system early in the morning. I found that the PO4 started to creep back up it was at 0.11 again. My next move is to clean out the canisters (which I neglected to do on Wednesday night); and clean out the skimmer head(s). I suspect the measurement will drop again, but will be sure to report back after the various phases of maintenance.
Alternatively, I was also hoping for an opportunity to test Tom's vile theory, so I might just do nothing for a period, see how far the levels rise up over a week or so, while I try to find a 10 micron filter sock kicking around (or something equivalent) so that I can collect a mechanically filtered vile sample.
The other thing I should note is that I noticed [yesterday morning] a fair amount of particulate floating/in suspended animation as the lights came on in the display tank (and immediately thought maybe Tom's onto something:fun5

. I don't often look that closely, but this could be a result of the scooter goby and mandarin goby kicking up detritus as they scour the liverock and sand for crustaceans.... or perhaps as Tom suggested it could be precipitates floating around. Now any reef tank with decent flow has a fair bit of detritus in suspension, but I'll have to pay closer attention to see if there are any notable differences between times of higher PO4 test results and Lower test results.
If there are any other angles y'all can think of that I should be experimenting with, please feel free to let me know and I'll be happy to attempt a scenario to validate it.
I think I'll let the reactor system run without cleaning out the particulates for a while; and try to test Tom's theory next. I might have an extra RO/DI prefilter canister kicking around that I can stick a 10 micron cartridge into for collecting test samples.
Oh and finally (almost forgot), the other change I made between the 0.04ppm reading of Wednesday night; and 0.11ppm reading of Friday morning was put the Calcium reactor back on line after topping up the media, and rinsing the the existing media (remember it was collecting precipitates for several weeks prior); and the single feed pump serves both the PO4 reactor system and the CaCO3 reactor independently (i.e. not in series this time); sooo - one of the consequences of this latest change is that the flow through the PO4 reactor system has been cut down by at least 50 - 70%. Quite possibly the PO4 could be leaching out or the liverock at a faster rate than the PO4 reactor can process it; or perhaps (just perhaps.. in light of all the argument against) if my original theory had a modicum of truth to it there is also the possibility (fully appreciative of Tom's objections) that weakly bonded PO4 precipitates stored up in that old CaCO3 media could in some way be contributing to the rise of total system PO4 among other factors... even though the CaCO3 reactor is no longer inline with the PO4 reactor system!
I'm aware of the objections, but just laying all of the thoughts on the table to be rolled into some kind/kinds of experiment(s) to see if they can be put to rest, no matter what side of reality they reside on...
Will let you know how it all goes in about a week or so.
Regards,
Sheldon