In situ Fe(III) coprecipitation from
Fe2+ oxidation
is a widespread phenomenon in natural environments and water treatment
processes. Studies have shown the superiority of in situ Fe(III) (formed
by in situ oxidation of a Fe(II) coagulant) over ex situ Fe(III) (using
a Fe(III) coagulant directly) in coagulation, but the reasons remain
unclear due to the uncertain nature of amorphous structures. Here,
we utilized an in situ Fe(III) coagulation process, oxidizing the
Fe(II) coagulant by potassium permanganate (KMnO4), to
treat phosphate-containing surface water and analyzed differences
between in situ and ex situ Fe(III) coagulation in phosphate removal,
dissolved organic matter (DOM) removal, and floc growth. Compared
to ex situ Fe(III), flocs formed by the natural oxidizing Fe2+ coagulant exhibited more effective phosphate removal. Furthermore,
in situ Fe(III) formed through accelerated oxidation by KMnO4 demonstrated improved flocculation behavior and enhanced removal
of specific types of DOM by forming a more stable structure while
still maintaining effective phosphate removal. Fe K-edge extended
X-ray absorption fine structure spectra (EXAFS) of the flocs explained
their differences. A short-range ordered strengite-like structure
(corner-linked PO4 tetrahedra to FeO6 octahedra)
was the key to more effective phosphorus removal of in situ Fe(III)
than ex situ Fe(III) and was well preserved when KMnO4 accelerated
in situ Fe(III) formation. Conversely, KMnO4 significantly
inhibited the edge and corner coordination between FeO6 octahedra and altered the floc-chain-forming behavior by accelerating
hydrolysis, resulting in a more dispersed monomeric structure than
ex situ Fe(III). This research provides an explanation for the superiority
of in situ Fe(III) in phosphorus removal and highlights the importance
of atomic-level structural differences between ex situ and in situ
Fe(III) coprecipitates in water treatment.