Poster Number 629
See more from this Division: S11 Soils & Environmental Quality
See more from this Session: Contaminants in Soil (includes Graduate Student Competition) (Posters)
Abstract:
Adsorption isotherm of Zn was fitted with Freundlich isotherm. Distribution coefficients for adsorption isotherms of Zn, KF(dm3 kg-1), increased as the amount of applied PFM increased. Greater KF suggests higher Zn adsorption capacity of the soil in the plow layer.
Metal-organic-complex-bound (Me-Org), exchangeable-with-CH3CO2Na (NaOAc) and water soluble-exchangeable (EXCH) Zn fractions of soils from 0-60cm deep layers under the TM and SM were significantly greater than those under the CHF. On the other hand, H2O2-extractable-organically-bound (H2O2-Org) fractions of the same layers were less than those under the CHF. Outer-sphere complex form with organic matter can not retain Zn strongly. Following to PFM decomposition, Me-Org, heavy metals associated with humic acid and fulvic acid in the soil, and H2O2-Org, heavy metals associated with persistent organic matter (ex. soil organic matter taken up by soil organisms) changed to be more mobile, EXCH and NaOAc extractable forms. Even though adsorption capacity of Zn may increase with PFM application, the greater amount of mobile Zn is likely to be moved downward by water percolation and moved laterally by surface water runoff after excessive and continuous application of PFM to the soil over a long time.
See more from this Division: S11 Soils & Environmental Quality
See more from this Session: Contaminants in Soil (includes Graduate Student Competition) (Posters)