Effect of Magnetic Zirconium/Iron-Modified Bentonite Addition on Phosphorus Mobilization and Species Transformation in River Sediments

Abstract

A magnetic zirconium/iron-modified bentonite (ZrFeBT) was prepared, and the effect of ZrFeBT addition on the mobilization and species transformation of P in river sediments was investigated using incubation sediment core experiments. The results showed that, under anoxic conditions, P could be released from river sediments into the pore water, and then P in the pore water could be released into the overlying water. The addition of ZrFeBT into river sediments could greatly suppress the release of P from river sediments into the pore water under anoxic conditions. Therefore, the release of P from the pore water into the overlying water could be significantly suppressed by the addition of ZrFeBT. After the addition of ZrFeBT into river sediments, the transformation of loosely sorbed P (Labile-P) and BD extractable P (BD-P) to NaOH extractable P (NaOH-rP) and residual P (Res-P) in the sediments was observed. The decrease of bioavailable P (BAP) including water soluble P (WSP), readily desorbable P (RDP), NaHCO3 extractable P (Olsen-P), algal available P (AAP), and Fe oxide-paper extractable P (FeO-P) in the sediments was also observed. A certain amount of P in the ZrFeBT after the incubation experiment was present in the form of mobile P (Labile-P and BD-P), Olsen-P, and FeO-P, which could be re-released into the pore water and overlying water when the environmental conditions change in the future. The control of P release from river sediment into the overlying water by the addition of ZrFeBT could be mainly attributed to the reduction of P in the pore water as well as the reduction of mobile P and BAP in the sediments after ZrFeBT amendment. The results of this study inidcated that ZrFeBT is a promising amendment for the regulation of P release from river sediments into the overlying water.