The
enrichment of geogenic phosphorus (P) in groundwater systems
threatens environmental and public health worldwide. Two significant
factors affecting geogenic P enrichment include organic matter (OM)
and Fe (oxyhydr)oxide (FeOOH). However, due to variable reactivities
of OM and FeOOH, variable strategies of their coupled influence controlling
P enrichment in groundwater systems remain elusive. This research
reveals that when the depositional environment is enriched in more
labile aliphatic OM, its fermentation is coupled with the reductive
dissolution of both amorphous and crystalline FeOOHs. When the depositional
environment is enriched in more recalcitrant aromatic OM, it largely
relies on crystalline FeOOH acting concurrently as electron acceptors
while serving as “conduits” to help itself stimulate
degradation and methanogenesis. The main source of geogenic P enriched
by these two different coupled processes is different: the former
is P-containing OM, which mainly contained unsaturated aliphatic compounds
and highly unsaturated-low O compounds, and the latter is P associated
with crystalline FeOOH. In addition, geological setting affects the
deposition rate of sediments, which can alter OM degradation/preservation,
and subsequently affects geochemical conditions of geogenic P occurrence.
These findings provide new evidence and perspectives for understanding
the hydro(bio)geochemical processes controlling geogenic P enrichment
in alluvial-lacustrine aquifer systems.