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Sammanfattning

The phosphorus (P) fraction distribution and formation mechanism in the supematant after P adsorption onto iron oxides and iron oxide-humic acid (HA) complexes were analyzed using the ultrafiltration method in this study. With an initial P concentration of 20 mg/L (I = 0.01 mol/L and pH = 7), it was shown that the colloid (1 kDa-0.45 gm) component of P accounted for 10.6%, 11.6%, 6.5%, and 4.0% of remaining total P concentration in the supematant after P adsorption onto ferrihydrite (FH), goethite (GE), ferrihydrite-humic acid complex (FH-HA), goethite-humic acid complex (GE-HA), respectively. The

Nyckelord

Phosphorus; Fraction; Ultrafiltration; Natural organic matter; Iron-DOM; Iron oxide-humic acid complexes

Publicerad i

Journal of Environmental Sciences
2017, volym: 55, sidor: 197-205
Utgivare: SCIENCE PRESS

SLU författare

UKÄ forskningsämne

Miljövetenskap

Publikationens identifierare

  • DOI: https://doi.org/10.1016/j.jes.2016.08.005

Permanent länk till denna sida (URI)

https://res.slu.se/id/publ/90498