Abstract: In the present study, the sorption of pyrene on two kinds of bulk
paddy soils, Gleyic Stagnic Anthrosols, and Ferric accumulic Stagnic Anthrosols
as well as their particle-size fractions was investigated. The sorption
isotherms fitted well with Freundlich equation. For both soils, the clay
fraction (<2μm) and coarse sand fraction (2000–250μm) had higher
sorption capacity than fine sand fraction (250–20μm) and silt fraction
(20–2μm). The logK_{oc} values obtained of each
soil and its particle-size fractions were similar, proving that SOM content was
a key factor affecting pyrene sorption. The Km_d values
showed a significant correlation with contents of dithionite-extractable Fe in
both paddy soils and a good relationship with CEC in Gleyic Stagnic Anthrosols,
indicating possible effects of surface properties of particle-size fractions on
the sorption of pyrene.