Solution 31P NMR Investigation of Inositol Hexakisphosphate Surface Complexes at the Amorphous Aluminum Oxyhydroxide–Water Interface

Phytate (myo-inositol hexakisphosphate, myo-IHP) is one of the most common organic phosphorus (P) species in soils and sediments which can be mineralized to increase the concentration of dissolved phosphate in pore water. Because of its six phosphate functional groups, functional group-specific adsorption mechanisms in reactive soil minerals become important in predicting solubility. In this study, solution 31P NMR was used to elucidate the functional group-specific adsorption mechanisms of myo-IHP at the amorphous Al hydroxide (AAH)-water interface at pH 6.5 in conjunction with batch adsorption experiments and Zetasizer measurements. The adsorption maximum of myo-IHP with AAH was ∼312.50 mmol kg-1, and the charge reversal effects in IHP-reacted AAH particles suggested the presence of inner-sphere surface species. The upfield shifts of various phosphate groups in the NMR spectra further supported the formation of inner-sphere IHP complexes at the AAH-water interface. When the initial myo-IHP/AAH (mol kg-1) was decreased from 2.5 to 1.25-1.67, P1,3 and P4,6 functional groups were coordinated in addition to P2; P5 became reactive with the ratio being decreased to <0.84, P5. This multifunctional group coordination increased aggregate size. The study showed that the availability of surface sites of adsorbents influenced the functional group-specific myo-IHP adsorption.