This question has been lingering around for years, and I haven't seen a clear answer yet -- and I don't have one either. A careful reading of the code should be able to answer this. I'd think Mike White would know off the top of his head, since he's worked so much on re-vamping some of the P transport, if I recall.
From the documentation, the hru and sub forms of P transported in overland runoff are the following:
hru SEDP = particulate mineral P, adsorbed to mineral particles
hru ORGP = particulate organic P
hru SOLP = dissolved mineral P
(no mention of dissolved organic P)
It seems that in the reaches, the common interpretation is that --
rch ORGP = particulate P, whether organic or mineral
rch MINP = dissolved mineral P
My working hypothesis is that, at the edge of the reach (conceptually), as the overland runoff enters the reach (stream) --
rch ORGP = hru ORGP + hru stable SEDP
rch MINP = hru SOLP + hru active SEDP
where active SEDP is the easily desorbed P from mineral grains, and stable SEDP is the less available P on the mineral grains.
***this is an assumption that should be checked!!***
In the stream water-quality documentation, there isn't much if any discussion of particulate mineral P. It seems that QUAL2E is considering mostly the uptake or release of nutrients by algal growth or decomposition, or sorption or desorption from bottom sediment (or perhaps they include suspended sediment), and settling of ORGP. It's unclear to me if ORGP includes algae or not, or whether ORGC is the labile C produced when algae decomposes...
I've avoided the issue by just dealing exclusively with total P, which is about the same as sticking my head in the sand.
It would be a significant contribution to this group if somebody would take a look at the code and come up with an answer, or if we could get Mike or Jeff to give us an answer on this one.
Sorry for the equivocal answer, but hopefully someone will be able to improve upon it. It's an important item to get cleared up.
Cheers,
-- Jim