Positive remediation on sedimentary P by combination of capping with calcium hydroxide and oxidation with perhydrol.

The capping is called passive remediation because the sedimentary P was released and then immobilized by the capping materials. However, the release depends on the environmental conditions. Therefore, a hypothesis was proposed that the oxidant was used to accelerate sedimentary P release and the capping material was used to capture those released P. It is positive remediation to reduce sedimentary P amount. The results show that soluble reactive phosphorus (SRP) concentration in the overlying water and pore water increased and then decreased gradually under the combination of sodium percarbonate (SPC) and Ca(OH)2, similar as that under the capping with single Ca(OH)2. The sedimentary P amount was reduced considerably and P concentration in the capping layer increased obviously after 60 days, compared with the capping with single Ca(OH)2. All these indicated that oxidation improved the sedimentary P release and the released P was captured and immobilized by the capping material of Ca(OH)2. However, the acceleration of sedimentary P release due to the oxidation is obviously different from the traditional mechanism that the oxic condition in the sediment is favor of the immobilization on sedimentary P. It is attributed to the oxidizability of ·OH from SPC. The reduction of mobile-P and the increase of Ca-P under the combined use are observed. This is similar as traditional mechanism of oxic condition. It is sure that positive remediation reduced sedimentary P amount, resulting in the decrease of P release risk in a long time.

Using sediment resuspension to immobilize sedimentary phosphorus.

The response of the transformation of internal phosphorus (P) to resuspended sediment was investigated in the sediment-water system under different disturbance intensity. The sediments and overlying water were collected from Taihu Lake, a typical shallow lake. The concentrations of particulate P (PP) and dissolved inorganic P (DIP) in the water phase and algal available P (AAP) and P fractions in the sediments and suspended particle characteristics were evaluated in laboratory-simulated experiments. The results show that dissolved oxygen (DO) in the overlying water increased continuously and pH decreased slightly under sediment resuspension. The concentration of ammonia nitrogen (NH4+-N) showed a distinct decline, indicating that sediment resuspension promotes the penetration of DO into the sediments. It was also favor of the formation of metal oxides and hydroxides, inducing soluble amorphous metal compounds oxidized to insoluble crystalline metal compounds under disturbance condition. This resulted in the increase of refractory P in sediment compared with the static conditions. Sediment resuspension is beneficial to long-term P retention. This can be confirmed by the increase of maximum P adsorption amount (Qmax) and the decrease of the degree of P saturation (DPS) and equilibrium P concentration (EPC0). This is the main explanation of DIP decrease in the overlying water. It is indicating that sediment resuspension not only improves the redox environment in the sediment-water system but also enhances P retention capacity.

[Environmental Significance of Phosphorus Fractions of Phytoplankton-and Macrophyte-Dominated Zones in Taihu Lake].

It is of great importance to study the environmental significance of phosphorus fractions in overlying water and sediments of typical phytoplankton-and macrophyte-dominated zones. It will help to clarify the process of phosphorus migration and transformation in the sediment-water interface, and has practical significance for understanding the eutrophication process and its treatment in different regions of Taihu Lake. The investigation was conducted within typical phytoplankton-and macrophyte-dominated zones of Taihu Lake over four seasons to analyze the spatial and temporal differences between phosphorus fractions in water and sediments, and reveal their environmental significance. The results showed that:① Total phosphorus (TP), total soluble phosphorus (DTP), dissolved inorganic phosphorus (DIP), and particulate phosphorus (PP) in the overlying water of phytoplankton-dominated zones were much higher than those in macrophyte-dominated zones. Most of them showed seasonal characteristics, which were higher in summer and autumn than in winter and spring. PP is the main component of TP, accounting for 71.8% to 89.6%. A similar distribution character was found in the content of chlorophyll (Chl-a) compared with phosphorus concentration in overlying water. ② The concentration of TP in the surface sediments of phytoplankton-dominated zones was 372.38-529.64 mg·kg-1, and that in macrophyte-dominated zones was 304.29-454.27 mg·kg-1. In surface sediments, concentrations of TP in phytoplankton-dominated zones were significantly higher than in phytoplankton-dominated zones. The highest TP concentrations appeared in winter, and the lowest in summer. These were owing to the input of exogenous pollution, and the migration and transformation of internal phosphorus between sediments and overlying water under different environmental conditions. ③ The order of the mass fraction of phosphorus in sediments was:NH4Cl-P < Fe-P < Org-P < Res-P < Al-P < Ca-P. Mobile-P=NH4Cl-P+Fe-P+Org-P, accounting for 9.10%-16.93% of TP in phytoplankton-dominated zones, and slightly higher in macrophyte-dominated zones, where it was 8.11%-13.50%. Res-P accounted for 10.06%-14.97% of TP in phytoplankton-dominated zones, and 11.02%-20.28% in macrophyte-dominated zones. The risk of internal phosphorus release in phytoplankton-dominated zones is high, which is not conducive to the fixation and burial of phosphorus. The eutrophication degree of different regions in Taihu Lake is obviously different, and different characteristics of phosphorus release and burial are showed. The phytoplankton-dominated zones deserve special attention because of their high internal phosphorus load and release potential.