Abstract

Previous research has demonstrated that biofilters are an effective technology for the removal of phosphorus (P) from stormwater. However, biofiltration is a relatively new technology and most field-scale systems are still fairly young, therefore little is understood about the long-term ability of biofilters to act as a sink for P. Studies from a board range of disciplines indicate that iron (Fe) and P interactions are an important mechanism for P sequestration in soils. To investigate long-term P retention dynamics and associations between Fe and P in biofilters we collected filter media cores from six biofilters in both Melbourne and Brisbane. The filter media was subjected to a four-step sequential extraction scheme designed to measure P associated with the following phases: i) Bioavailable P; ii) P-adsorbed to iron oxyhydroxides; iii) P associated with amorphous iron oxyhydroxides; and iv) Organic P. The results suggest that P accumulation varies spatially (areally and with depth) in biofilters. P concentrations were highest in the top 10 cm of the filter media and near stormwater inlets. In all biofilters tested, surface layer P was mostly associated with the amorphous Fe and organic phase, which is largely related to the build-up of trapped sediment. P concentrated in the Fe-adsorbed phase increased at lower depths suggesting that Fe-P sorption interactions may play an important role in long-term P retention. This result emphasises the importance of maintaining good hydraulic performance in biofilters, since Fe-adsorbed P may be sensitive to changes in redox potential, leading to release under reducing conditions. These findings may influence how we design biofilters and plan system maintenance to ensure effective long-term P removal.

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Last updated: 11th Apr 2017