[Efficiency of Magnesium Hydroxide Capping and Amendment to Control Phosphorus Release from Sediments].

Eutrophication of freshwater bodies has become a global environmental problem, and phosphorus (P) has been identified as one of the key limiting factors responsible for this eutrophication problem. Reducing internal P release is crucial to the control of the eutrophication of freshwater bodies besides reducing the input of external P. To control sedimentary P release, magnesium hydroxide[Mg(OH)] was applied as a capping and amendment material in this study. The adsorption performance of phosphate on Mg(OH) was investigated in batch mode, and the effect of Mg(OH) capping and amendment on the mobilization of P in sediments was studied using sediment incubation experiments. Results showed that Mg(OH) exhibited good adsorption performance toward phosphate. The phosphate removal efficiency of Mg(OH) increased with increasing adsorbent dosage. The adsorption equilibrium data of phosphate on Mg(OH) could be better described by the Freundlich and Dubinin-Radushkevich isotherm models compared to the Langmuir isotherm model. Mg(OH) capping and addition both could effectively control the release of reactive soluble P (SRP) from sediments into the overlying water, resulting in a low concentration of SRP in the overlying water under Mg(OH) capping and amendment conditions. Mg(OH) capping and amendment both could reduce pore water SRP in the uppermost sediment (0-10 mm), which played a key role in the control of the release of SRP from sediments into the overlying water. The as-prepared Mg(OH) possessed a much higher phosphate adsorption ability than commercial Mg(OH), and the former also had a higher controlling efficiency of sedimentary P release than the latter. In summary, Mg(OH) is a promising capping and amendment material for the control of internal phosphorus release in freshwater bodies.