Phosphorus speciation in agricultural catchment soils and in fresh and dried sediments of five constructed wetlands

← Takaisin
Tekijä Laakso, Johanna; Uusitalo, Risto; Yli-Halla, Markku
Sarja Geoderma
DOI/ISBN-numero http://dx.doi.org/10.1016/j.geoderma.2016.02.007
Päivämäärä 2016
Avainsanat agricultural catchments, constructed wetlands, phosphorus, sediment
Rahoitus Salaojituksen Tukisäätiö sr
Organisaatio University of Helsinki
Sivut 18 - 26
Volyymi 271
Kieli englanti
Saatavuus http://www.sciencedirect.com/science/article/pii/S001670611630057X

Constructed wetlands and ponds (CWs) are installed to trap suspended material and particulate phosphorus (P) in agricultural runoff. This study investigated whether the P speciation and P sorption capacity of source soils differ from those of CW sediments and whether drying of dredged sediment changes its characteristics. Samples collected from five agricultural CW sites in south-west Finland, two with chemical-aided (aluminium chloride and ferric sulphate) P precipitation and all representing fine-textured mineral soils, were analysed for various P plant availability indices. Clay contents of the CW sediments were much higher than in catchment soils, likely because of selective erosion. All CW sediments were characterised by similar total P content but clearly higher content of anion exchange resin-extractable P in fresh sediments than the source soils. In general, sediment content of NH4F-extractable (aluminium (Al)-associated) P was significantly lower and NaOH-extractable (iron (Fe)-associated) significantly higher than in source soils. Reduced conditions, conducive to mobilisation of Fe-associated P, were observed in all CWs. Accumulation of sulphur (S) in sediments and a pH decline of up to two units upon drying suggested presence of Fe sulphides. Drying also increased oxalate-extractable Al and Fe (hydr)oxide content by 9–47%, resulting in lower degree of P saturation. These results indicate that dredged CW sediments differ greatly in their P retention characteristics from their parent soils. Returning CW sediments to fields is likely to decrease the amount of readily available P for crop uptake.