The effects of sediment aluminum(Al),organic carbon(OC),and dissolved oxygen(DO)on phosphorus(P)transformation,at the water-sediment interface of a eutrophic constructed lake,were investigated via a series of simulati...The effects of sediment aluminum(Al),organic carbon(OC),and dissolved oxygen(DO)on phosphorus(P)transformation,at the water-sediment interface of a eutrophic constructed lake,were investigated via a series of simulative experiments.The above three factors had various influences on dissolved P concentration,water pH,water and surface sediment appearance,and P fractions.Additions of Al had the greatest effect on suppressing P release,and the water p H remained alkaline in the water-sediment system under various OC and DO conditions.No dissolution of the added Al was detected.31P-N M R characterization suggested that OC addition did not promote biological P uptake to polyphosphates under oxic conditions.The simulation result on the added phytate indicated the absence of phytate in the original lake sediment.As compared to the reported natural lakes and wetland,the water-sediment system of the constructed lake responded differently to some simulative conditions.Since Al,OC,and DO can be controlled with engineering methods,the results of this study provide insights for the practical site restorations.展开更多
基金This study was supported by the National Key Research Project on Water Environment Pollution Control in China(Nos.2012ZX07301 and 2017ZX07202002).
文摘The effects of sediment aluminum(Al),organic carbon(OC),and dissolved oxygen(DO)on phosphorus(P)transformation,at the water-sediment interface of a eutrophic constructed lake,were investigated via a series of simulative experiments.The above three factors had various influences on dissolved P concentration,water pH,water and surface sediment appearance,and P fractions.Additions of Al had the greatest effect on suppressing P release,and the water p H remained alkaline in the water-sediment system under various OC and DO conditions.No dissolution of the added Al was detected.31P-N M R characterization suggested that OC addition did not promote biological P uptake to polyphosphates under oxic conditions.The simulation result on the added phytate indicated the absence of phytate in the original lake sediment.As compared to the reported natural lakes and wetland,the water-sediment system of the constructed lake responded differently to some simulative conditions.Since Al,OC,and DO can be controlled with engineering methods,the results of this study provide insights for the practical site restorations.