Maybe not precipitation but I would imagine the surface area would be a colonization zone for the bacteria consuming the PO4.
This assumes that the said bacteria that colonized the surface and consumed the PO4 are washed into suspension before processing.
No idea what the protocols are for these tests so I may be completely off base here. Either way, I would just pick one test, standardize my process, and stick with it.
I use the Hanna and have always wondered how much variability the powder adds to my results. I pre-dump it onto folded filter paper, then use a funnel to add to the sample but I'm pretty sure I never get 100% of the powder into the sample.
To be honest I do not believe in significant precipitation that makes the po4 stay in the sample vial. Precipitates will also release all P in 10000K and on vial surface there will be no significant precipitation.
And all po4 that have been transformed as organic P like inside bacterial cells, algue or whatever will also be 100 % released in the 10000K plasma. So icp oes is not sensitive to transport or time in sample.
So back to thread: its very unlikely an icp is that much off, especially not in that direction, so main hypothesis must be its your manual tests and Trident NP that is off. BUT To be sure, measure with a ref fluid. If you after thar find the manual tests ARE correct, then we have just a seldom exception where something went wrong in that particular ICP test.
I have sent in many icp tests and always compare the icp calculated po4 with true photometric measurements. If you filter the water with 0
22û then no bacteria will come into sample. During those circumstances the calculated icp po4 is close to true photometric po4.
With no filtering the difference can be more, like 100% difference between true po4 and icp calculated as in those cases bacteria will consume true po4 but icp calculated will ofcourse still be the same as icp measure p atoms.