Efficiency and mechanism of controlling phosphorus release from sediment using a biological aluminum-based P-inactivation agent

Abstract

Eutrophication is a significant challenge for surface water, with sediment phosphorus (P) release being a key contributor. Although biological aluminum-based P-inactivation agent (BA-PIA) has shown effectiveness in controlling P release from sediment, the efficiency and mechanism by BA-PIA capping is still not fully understood. This study explored the efficiency and mechanism of using BA-PIA capping controlling P release from sediment. The main mechanisms controlling P release from sediment via BA-PIA capping involved transforming mobile and less stable fractions into stable ones, passivating DGT-labile P and establishing a 13 mm 'P static layer' within the sediment. Additionally, BA-PIA's impact on Fe redox processes significantly influenced P release from the sediment. After BA-PIA capping, notable reductions were observed in total P, soluble reactive P (SRP), and diffusive gradient in thin-films (DGT)-measured labile P (DGT-labile P) concentration in the overlying water, with reduction rates of 95.6%, 92.7%, and 96.5%, respectively. After BA-PIA capping, the diffusion flux of SRP across the sediment-water interface and the apparent P diffusion flux decreased by 91.3% and 97.8%, respectively. Additionally, BA-PIA capping led to reduced concentrations of SRP, DGT-labile P, and DGT-measured labile Fe(II) in the sediment interstitial water. Notably, BA-PIA capping significantly reduced P content and facilitated transformation in the 0∼30 mm sediment layers but not in the 30∼45 mm and 45∼60 mm sediment layers for NaOH-extractable inorganic P and HCl-extracted P. These findings offer a theoretical basis and technical support for the practical application of BA-PIA capping to control P release from sediment.